remote sensing UAVs for Science in Antarctica

: Remote sensing is a very powerful tool that has been used to identify, map and monitor Antarctic features and processes for nearly one century. Satellite remote sensing plays the main role for about the last ﬁve decades, as it is the only way to provide multitemporal views at continental scale. But the emergence of small consumer-grade unoccupied aerial vehicles (UAVs) over the past two decades has paved the way for data in unprecedented detail. This has been also veriﬁed by an increasing noticeable interest in Antarctica by the incorporation of UAVs in the ﬁeld activities in diversiﬁed research topics. This paper presents a comprehensive review about the use of UAVs in scientiﬁc activities in Antarctica. It is based on the analysis of 190 scientiﬁc publications published in peer-reviewed journals and proceedings of conferences which are organised into six main application topics: Terrestrial, Ice and Snow, Fauna, Technology, Atmosphere and Others. The analysis encom-passes a detailed overview of the activities, identifying advantages and difﬁculties, also evaluating future possibilities and challenges for expanding the use of UAV in the ﬁeld activities. The relevance of using UAVs to support numerous and diverse scientiﬁc activities in Antarctica becomes very clear after analysing this set of scientiﬁc publications, as it is revolutionising the remote acquisition of new data with much higher detail, from inaccessible or difﬁcult to access regions, in faster and cheaper ways. Many of the advances can be seen in the terrestrial areas (detailed 3D mapping; vegetation mapping, discrimination and health assessment; periglacial forms characterisation), ice and snow (more detailed topography, depth and features of ice-sheets, glaciers and sea-ice), fauna (counting penguins, seals and ﬂying birds and detailed morphometrics) and in atmosphere studies (more detailed meteorological measurements and air-surface couplings). This review has also shown that despite the low environmental impact of UAV-based surveys, the increasing number of applications and use, may lead to impacts in the most sensitive Antarctic ecosystems. Hence, we call for an internationally coordinated effort to for planning and sharing UAV data in Antarctica, which would reduce environmental impacts, while extending research outcomes.


Introduction
The importance of remote sensing for the knowledge of Antarctica became immediately evident after the development of the first airplane flights in the late 1920s, which allowed discovering more of the hinterland than all previous surveys during the preceding century. The first flight in 1929 by Hubert Wilkins taking off from Deception Island, unveiling much of the northern part of the Antarctic Peninsula, was a milestone [1]. Afterwards, the attempts to make a trans-Antarctic flight, namely the most notable one in 1935 by Herbert Hollick-Kenyon and Lincoln Ellsworth, which achieved the first crossing of the continent from Dundee Island to the Ross Ice-Shelf, revealed the existence of the Trans-Antarctic Mountains [2]. Both of these expeditions allowed taking many photos which, although oblique and not always well geolocated and therefore not adequate for precise mapping, constitute the first remote views of the Antarctic continent.
The systematic cartography with aerial photography started only after the end of the second world war, first with the Ronne Antarctic Research Expedition (RARE) followed about one decade later by the Falkland Islands Dependencies Aerial Survey Expedition (FIDASE) [3]. But it was only after the launching in 1972 of the first civilian satellite ERST-1 (later renamed to Landsat1) that the gate to the spaceborne Earth Observation would finally be open and change definitely the human view of planet Earth. This is particularly evident for Antarctica with the availability of almost global mosaics soon after [4,5]. These products were enhanced some three decades later with the Landsat Image Mosaic of Antarctica (LIMA) built after many images at the typical 30 m resolution of these platforms [6]. Several other complete products built after satellite remote sensing are becoming available like, for instance, the elevation model of the continent named REMA-The Reference Elevation Model of Antarctica [7] with a spatial resolution of 10 m, built after photogrammetric techniques.The surface elevation, ice-thickness and subglacial bed elevation for the whole continent, derived with data from a variety of remote sources, are also available in the product Bedmap2 [8]. The mapping of terrestrial or ice-free areas is obtainable at a resolution of 30 m after Landsat imagery [9]. In another different topic, the remote identification of penguin colonies at continental scale started to be possible by looking at the faecal stains [10].
It means that global views of Antarctica, provided by the above mentioned satellite datasets, are already available for several features or properties of interest. But many relevant details, identified at ground level by traditional field surveys, are not yet perceived for regional or continental-scale areas, even with the most recent satellite data of very high-resolution. The bridging of those two scales by Unoccupied Aerial Vehicles (UAVs) allows perceiving most of the details observed on the ground and covering larger areas. In addition, these systems can also be used beyond surface features, namely to better exploit the atmosphere dynamics and properties for complementing current techniques and procedures. Also, UAVs can play a remarkable role in inventorying and monitoring wildlife in a more extended and comprehensive way with minimal animal disturbance. These systems are also very flexible and can be equipped with an increasing variety of light-weight sensors, also allowing their regular use often below cloud covers. Therefore, like in many other disciplines and in other regions, the benefits to obtain after UAV surveys in Antarctica are evident as they are able to provide the acquisition of remotely sensed data with unusual detail, more frequently and in safer and cheaper ways.
The rapid worldwide growth of use of UAVs in the last decade has taken Antarctic Treaty Parties to recognise their importance for obtaining additional and more detailed data in the continent. It naturally pushed them to evaluate the environmental impacts and also to start establishing guidelines for their use in the field. These practical rules were first elaborated by the Council of Managers of National Antarctic Programs (COM-NAP) and presented at the 39th Antarctic Treaty Consultative Meeting (ATCM) held in 2016 [11]. Several improvements of the document were performed until 2021, which, so far, consists of the most definitive version of the Antarctic Remotely Piloted Aircraft Systems (RPAS) Operator's Handbook [12]. This document contains the guidance to ensure the safe operation of UAVs and to minimise the risks for environmental impacts in the Antarctic Treaty Area.
The last decade has seen a notorious increase of the use of UAVs in Antarctic research. This is evident on the growing number and diversity of publications in journals and presentations in conferences, but a comprehensive review is missing. The generic reviews published in the last years on the use of UAVs in scientific research [13][14][15] do not pay the adequate attention to Antarctic activities, indicating very few references. Although widening this panorama, the more recent and focused reviews on polar and cryosphere subjects [16,17] do not yet provide a broad view of the use of these platforms in Antarctica.
It seems, therefore, the right time to comprehensively report what has been developed so far and to identify future prospects in important research topics not yet addressed about the use of UAVs in Antarctica.

Search for Published Documents and Methods
The search and selection of publications that include UAVs in the research activities in Antarctica was only focused in full papers published in journals, conference proceedings and chapters of books, since are the only ones able to provide complete descriptions of the research. Therefore, abstract conferences and similar brief documents were disregarded and not selected for inclusion.
The search for scientific publications started with the generic search engines Web of Science and Google Scholar with a combination of the keywords: 'Antarctica', 'polar', 'UAV', 'UAS', 'RPAS', 'unmanned/unoccupied aerial vehicles', 'unmanned/unoccupied aerial systems', 'remotely piloted aircraft systems' and 'drones'. The manual verification of the adequacy of the references and the filtering of false positives was followed by an additional effort to look for possible missing and less obvious references through more specific searches. This comprised searches on the sites of the publishing companies editing journals on polar, cryosphere, Antarctic and related research. Finally, the search was tightened by cross-checking the list of references of the selected publications, which allowed to identify some additional papers published in conference proceedings.
The list of 190 publications found under these conditions contains the results of searches carried out until the end of February 2022. Each of these was scrutinised about the research topic and objectives, the location of the surveys, equipment, data and results.
For the sake of clarity and organisation, it was decided to group the publications around six thematic subjects or application topics that practically cover the whole range of research activities in Antarctica: Terrestrial encompassing vegetation, landforms, soils and related topics in ice-free areas, Ice and Snow for the quantification and monitoring of solid water features, Fauna about the inventorying and monitoring of animal wildlife, Technology related to the design, development and testing of dedicated UAV platforms and sensors for use in the austral extreme environments, Atmosphere for the research in atmospheric and meteorological studies and Others to encompass varied matters not fitting in any of the previous categories and related to legislation, field protocols or inquiries to Antarctic researchers using UAVs.
The assignment of a category to each paper was straightforward for the large majority of them. In those few items where multiple and intermingled topics were addressed and the decision less obvious, like for instance between Snow and Ice and Atmosphere, or Technology and Snow and Ice, the assignment was based on the predominant or more developed topic on the paper.
A preliminary synthesis showing a first snapshot about the use UAVs in Antarctica is presented in Section 3, being the breakdown analysis of the scientific activities by each topic presented in Section 4.

A First Snapshot
The first paper describing the use of a UAV in Antarctic research was published in 2006, describing the technological development of specific systems for operating in the southern polar continent [18]. The annual distribution of published papers in the following period of 16 full years till 2021 shows a clear growing trend (Figure 1), stable in the first years, but more evident after the peak of 2014 and with a clear jump after 2019. This growing trend seems to be kept in 2020 and 2021, the years with the higher number of publications on the subject under review. The five papers published so far in 2022 are used in all counts but not included in the previous figure. More than three-quarters of the publications correspond to papers in scientific journals and more than one-quarter to proceedings of conferences, with the rest, with a small expression, published in chapters of books and magazines, as detailed in Table 1.  (Springer, eISSN-1432-2056 with 12 papers. They are followed with only 5 papers by Scientific Reports (Nature Research, eISSN-2045-2322) and with 4 papers each by Antarctic Science (Cambridge University Press, eISSN-1365-2079), Antarctic Record (National Institute of Polar Research-Japan, eISSN-2432-079X) and Earth System Science Data (Copernicus Publications, eISSN-1866-3516). These 6 journals, which contain about a bit less than one third of the articles (42 papers), are therefore the main preferences to publish UAV based research in Antarctica. The other more than two thirds (105 papers) are dispersed by 80 other regular publications, indicating wide possibilities to publish methodologies and results. It should be also highlighted that most of the journals are of international circulation and included in Web of Science (74 titles, 86%) and Scopus (77 titles, 90%). Consequently, the fraction of papers included in these two databases is also very high: 89% (131 papers) are part of Web of Science and 93% (136 papers) of Scopus. The 36 papers in proceedings are mostly related to remote sensing conferences (15 publications), aeronautics, robotics and similar (9 publications). The other 12 publications are presented in a large variety of conferences related to the environment, meteorology, permafrost, polar regions, geomorphology or geophysics.
The pair of magazine publications is related to Eos, the science news publication of the American Geophysical Union that includes relatively lengthy and informative descriptions of on-going research, therefore acceptable to be included in this review.
The distribution of the 190 publications by these 6 categories is shown in Table 2. The global evaluation shows that two out of the six categories, Terrestrial (28.4%) and Ice and Snow (23.7%), assume the higher relevancy with more than half of the publications. They are followed by Fauna (20.5%), Technology (14.2%) and Atmosphere which, although a bit less frequent, can still be considered relevant accounting for 10.6% of the papers. Finally, Others includes only a few but wide-range references on the topic. UAVs are being currently used in almost every location of Antarctica where regular research is being performed, mostly closer to the scientific stations in land, but also after vessel expeditions at sea. The location of the surveys is presented in the map of Figure 2a, showing a major concentration in the northern Antarctic Peninsula, especially in the South Shetlands (Figure 2b), where Terrestrial and Fauna topics predominate. This higher number of surveys can be related to an easier and more frequent access to the field in a region with more stations and more frequent marine expeditions. A second hot spot for UAV surveys is found at Terra Nova Bay, where several scientific stations are also established, but where Atmosphere studies predominate. The other surveys are developed close to scientific stations along the East Antarctic continental coastal areas and nunataks and related to Ice and Snow, Terrestrial, Fauna and Atmosphere topics. The surveys in ocean expeditions are mostly addressing Atmosphere studies. The development of the research activities in Antarctica is a strong collaborative endeavour, normally involving multidisciplinary teams of several people from different institutions and countries. A simple statistical analysis reveals the number of authors per paper to be on average equal to 5.3 and the mode equal to 5, while the number of authors per paper varies between 1 and 24 authors (Figure 3). But as a whole, about 95% of the publications show up to 10 authors. The first authorship of a paper is considered a relevant factor to evaluate gender disparity [25]. Usually, the first author is the researcher of a group who has made most of the efforts and receives most credit for the publication [26]. Therefore, we considered it to be a good starting point to make a preliminary evaluation on this review. We determined the gender of the first author by their first name. In the cases were the author gender was unclear, we consulted the institutional websites listing the publications and internet search engines to look for biographical sketches. The gender of the first author of the 190 publications was performed without ambiguity. The evaluation of first authorship gender in each publication shows that 76% of the first authors are male [27]. Although a near parity is observed in the early years of the evaluation period, the number of papers published by then was very small (2 in 2007 and 5 in 2008). Anyhow, the more recent trend seems to show a decrease in the gender gap ( Figure 4), but this last period of two full years is yet too short to derive a conclusive bridging effect. It is worth analysing this distribution by topic of research, since distinct results are observed, as shown in Table 3. There is a strong unbalance in most topics, namely in Technology and Others, with all publications lead by male authors, but also on Terrestrial with a ratio of 5:1. A less unbalanced relation is shown in the topics Ice and Snow and Fauna with 2.2:1 and 2.3:1 proportion, respectively. The only topic where male authors do not predominate is in Atmosphere where the parity 1:1 is reached. Table 3. Gender of the 1st author of each publication. Terrestrial  45  9  83-17  Ice and Snow  31  14  69-31  Fauna  27  12  69-31  Technology  27  0  100-0  Atmosphere  10  10  50-50  Others  5  0  100-0   Total  145  45  76-24 Concerning the geographical origin of the institution of the first author of the paper, they originate from 29 countries of all continents ( Table 4). The more prolific, with more than 10 papers in leading authorship, are the United States of America (38 publications), Poland (20 publications), Russia (18 publications), Australia (15 publications), Germany, China and Japan (13 publications each), and the United Kingdom (12 publications).  (1) Oceania (22) Australia (15) and New Zealand (7) The number of collaborations between institutions from different countries is relatively low when it comes to publish the results of the research activities, as shown in Table 5. Although the transnational cooperation originates publications with authors coming from up to four countries (in Terrestrial, Fauna and Atmosphere), in the largest majority of them the authors belong to one single country (74.2%). The weight of multi-country authorship is inversely proportional to the number of countries involved: papers with authors from 2 countries correspond to 16.9%, from 3 countries to 6.3% and from 4 countries just to 2.6%. This result is practically the same in each application topic. The number of bibliographic references of this article cited in previous articles was also counted. The cross-references are in general incipient: one common reference with Colomina and Molina (2014) [13] and Yao et al. (2019) [15], five with Bhardwaj et al. (2016) [16] and seven with Pajares (2015) [14]. Only in the very recent UAV review by Gaffey and Bhardwaj (2020) [17], also of more related topics, this number gains a certain expression through the 20 common references found.

Application Topics
The analysis of the 190 references is performed by application topic, being each one also organised in sub-topics around similar subjects and objectives. The sequence of presentation and discussion is based on the decreasing number of papers constituting each topic: Terrestrial (54 papers), Ice and snow (45 papers), Fauna (39 papers), Technology (27 papers), Atmosphere (20 papers) and Others (5 papers).

Terrestrial
The applications in the terrestrial or ice-free areas are varied and constituted by 54 papers, references [21][22][23], with most of them focused on vegetation (20 papers) and landforms and soils (18 papers) as shown in Table 6. The other sub-topics of interest refer to reference datasets like orthomosaics and elevation models (12 papers), typical from the early UAV surveys in Antarctica, together with geophysical surveys (3 papers) and the development of image processing algorithms (1 paper). Table 6. Terrestrial applications using UAVs in Antarctica (54 papers).

Main Topic Specific Topic References
Vegetation (

Vegetation
Mapping: The lack of detail of satellite imagery to identify the small and sparse patches of vegetation, even at sub-metric scales, pushed the early UAV surveys to obtain products with ultra-high resolution. Therefore, the first mapping attempts of moss beds by Lucieer et al. (2010Lucieer et al. ( , 2011 [28,29] in the Windmill Islands region, East Antarctica, allowed building ortho-mosaics and Digital Elevation Models (DEM) with 1-2 cm resolution, but also providing the first Structure-from-Motion (SfM) procedures to process cloud points with adequate georeferencing after ground-control markers installed in the field as reported by Turner et al. (2012) [30]. The use of thermal, multi and hyperspectral cameras by Lucieer et al. (2012 [31,32] allowed them improving the identification of moss beds and to start assessing their health condition. In addition, the experience gained by this team, demonstrated in the previous references, led to the building of accurate microtopography of moss beds, which was used to simulate water availability from snowmelt and to correlate with moss health conditions (Lucieer et al., 2014 [33]). The identification of other types of vegetation was also achieved with only RGB imagery, especially due to the spatial details provided by the ultra-high spatial resolutions, like shown for cyanobacterial mats in datasets captured with a fixed-wing platform in surveys in McMurdo Valleys by Brollard-Breen et al. (2015) [34]. The discovery and mapping of a large population of a liverwort type also become possible after surveys with a RGB camera by Putzke et al. (2020) [35] in Nelson Island, South Shetlands. Similarly, the identification of vegetated and non-vegetated surfaces after UAV-based mosaics was correlated with permafrost active layer conditions obtained after electric resistivity surveys in Barton Peninsula, South Shetlands (Kim et al., 2020 [36]). The evaluation of the adequacy of NDVI-Normalised Difference Vegetation Index to discriminate main vegetation types (lichens, mosses and algae) in satellite imagery (Sentinel-2 and Landsat) was fully exploited after UAV surveys in Hope Bay, Antarctic Peninsula by Sotille et al. (2020) [37], in which they proposed a categorisation of this vegetation index in interval ranges more likely to contain a given vegetation cover. The ability of RGB-based vegetation indices to discriminate their main types after UAV surveys is evaluated by Váczi et al. (2020) [38] with the help of multispectral ground-truthing built after hand-held spectrometer surveys. The UAV survey of a moss carpet, transplanted to a neighbourhood area to minimise the impact of the reconstruction of the Brazilian station in King George Island, helped Câmara et al. (2021) [39] to make its characterisation and verify the health condition after a three-year period. Bollard et al. (2022) [40] developed aerial surveys with UAV in three protected areas in the Ross Sea region to create very detailed maps of vegetation using a multispectral camera, reinforcing the environmental and conservation benefits obtained with this kind of operations.
Health assessment: The health assessment of mosses is described in detail by Turner et al. (2014Turner et al. ( , 2018 [41,44], also correlating it with the availability of water from upstream snowbanks, only possible to obtain through the exploitation of the micro-topography obtained after the UAV surveys (Lucieer et al., 2014 [33]). But the identification of the health condition of mosses using imaging spectroscopy required its previous evaluation in laboratory experiments (Malenovský et al. (2015) [42]), by deriving stress-indicating traits after visible and near infrared reflectance in a nonlinear machine learning regression. The stress indicators selected (turf chlorophyll a+b and leaf density) were afterwards assessed on mosses on hyperspectral images of centimetre spatial resolution after UAV surveys (Malenovský et al., 2017 [43]), which helped in providing timely and spatially explicit warnings of environmental stress events. More recently, with the goal of optimising field surveys with more efficient data acquisition procedures, Turner et al. (2019) [45] made an assessment of optimal resolutions (spectral and spatial) of multiple sensors (multi and hyperspectral) to identify up to which degree the quantitative mapping of physiological health indicators of moss blankets is reliable.
Change detection: The detection of changes in vegetation is greatly helped with the details provided by UAV surveys. The accurate discrimination between lichen and moss formations at centimetre resolutions by Miranda et al. (2020) [46] in King George Island, South Shetlands plays a key role in designing and calibrating robust machine learning classifiers of synchronous and previous satellite imagery (WorldView) to detect detailed changes along a recent decade. In another field assessment in the McMurdo Dry Valleys to characterise inter-annual changes in microbial mats, Levy et al. (2020) [47] evaluated through intensive detailed testings the necessary characteristics that the mapping based on UAV surveys with a hyperspectral point spectrometer should have to make meaningful multitemporal evaluations.

Landforms and Soils
Moraines and glacier fronts: The mapping of moraines was performed to characterise their extent and topography but also, and more specifically, to obtain clast size distributions across the surface, as described by Westoby et al. (2015) [48]. The inter-annual evolution of moraine surfaces was also quantified by the same team led by Westoby et al. (2016) [49] making the integration of multitemporal DEMs obtained after UAV and Terrestrial Laser Scanning (TLS) surveys, which, due to their fine-resolution, allow detecting topographical changes over short time periods. The link between these two type of surveys (aerial and ground) is better and more detailed established by Woodward et al. (2022) [50] to understand the dynamic processes involved in the formation of blue-ice moraines. The chronology of blue ice moraines in Queen Maud Land is also established by Akçar et al. (2020) [51] using surface exposure dating with multiple cosmogenic nuclides of boulders, guided by the photogrammetric products after UAV surveys. The current retreat of glaciers allows identifying, mapping and quantifying the glacial and periglacial landforms developed in the proglacial zone with a very high detail after UAV-based products (image mosaic and DEM) like presented by Kreczmer et al. (2021) [52] in the Warszawa Icefield, King George Island.
Patterned ground: The mapping of patterned ground, namely sorted stone circles, can only be performed by remote sensing through ultra-high resolution datasets. This was achieved with the image mosaics and specially with the elevation datasets of mmcm resolution in Barton Peninsula ( [53]. The automated processing based on machine learning algorithms allowed making adequate identifications and delineations of thousands of individual circles on large datasets, enriching the characterisations and improving the statistics of the traditional field measurements. Other: The mapping of landforms around the West Antarctica Ice-Sheet (WAIS), performed through satellite imagery and traditional field work, was much enriched with the details provided by a TLS and UAV imagery in areas of complex debris accumulations, like reported in a couple of papers by   [54,55]. The level of detail of the mapping after UAV surveys, in the scale and amount of features, can be very high, creating comprehensive legends of periglacial features, for instance, solifluction landforms, scarps and taluses, patterned ground, coastal landforms as cliffs and beaches, landslides and mud flows, and stone fields and bedrock outcrops, as detailed by Dąbski et al. (2017) [56]. The development of beyond visual line of sight flights (BVLOS) permits surveying more distant areas of interest in multigoal missions, which, after the creation of image mosaics and DEM with centimetre resolutions, allowed making the mapping of varied landforms (volcanic, mass movements, fluvial, aeolian and coastal), identifying the communities of vegetation (mosses, lichens and grasses) and also inventorying the fauna, namely, penguin rookeries and individual pinnipeds in the South Shetlands as reported by Zmarz et al. (2018) [57]. Similar surveys and derived data products obtained by Dąbski et al. (2020) [58] were also the basis to map landform assemblages developed in the forelands of glaciers with a detail and extension not possible from satellite imagery nor from field work. The detailed mapping of geomorphological slope processes related to snow patches after UAV surveys and field observations in James Ross Island, East Antarctic Peninsula, are detailed by Kňažková et al. (2021) [59], allowing this team to discuss the role of snow related processes as landscape-shaping factors. Another type of landforms, whose full details are only observable at the scale of UAV datasets, are permafrost mounds and in particular frost blisters, whose multitemporal size variations were quantified by Ponti et al. (2021) [60] for assessing the sublimation rates on perennially frozen lakes and water supply mechanisms.
Soils: The extrapolation of the optical signatures of the surfaces obtained after field data to the visible imagery of UAV surveys allowed Mergelov et al. (2020) [61] to classify the spatial distribution of biological soil crust (BSC) classes and other landscape components and, consequently, to understand how organic carbon enters depauperate soils and contributes to the carbon reservoir of the topsoil. To examine poorly understood linkages of microbial communities between lake ecosystems and surrounding soils and glaciers, as to provide the context of the fieldwork area and discriminate different classes (moraines, glacier/lake ridge, ice patch within lake) and to guide the sampling of microbial communities in cryoconite holes, UAV surveys developed in Lake Untersee Oasis in Queen Maud Land, East Antarctica played an important role as reported by Weisleitmer et al. (2020) [62]. The analysis of soils in a recent glacier retreat front was guided by UAV surveys that allowed reconstructing successional stages with very detail, as reported by Gyeong et al. (2021) [63]. The role played by the ornithogenic factor in soil formation in Antarctica was analysed by Abakumov et al. (2021) [64] on field and laboratory data on soil features and also on UAV imagery to help identifying different soil areas and field routes.

Basemaps
Mosaics and DEM: In the terrestrial areas without detailed maps, the initial UAV surveys were naturally more focused in obtaining adequate imagery and in testing different operational procedures to help building the best reference products, than in extracting meaningful information for any specific topic of research. The verification of the detail that could be extracted from distinct surfaces like vegetation, bare soil and rock, and also patterned ground, was primordially analysed by Bandeira et al. (2014) [65], similarly to what was attained in moraines, polygonal networks and snow patches by Suganuma et al. (2016Suganuma et al. ( , 2017 [66,67]. The systematic surveys in areas of few tens of km 2 , describing in detail the operational procedures adopted to obtain the mosaics and DEM, are good examples achieved by Kim et al. (2014) [68] in the entire ice-free area of Barton Peninsula and by Lamsters et al. [69] for the largest eight Argentine Islands located in the Western Antarctic Peninsula and in surveying not only their terrestrial areas but also the ice caps. The creation of basemaps, specially detailed DEM, also played an important role in the quantitative procedures developed by the Antarctic Program of Colombia to find the most adequate location for building their new station in the South Shetlands, as shown by Coronado-Hernández et al. (2020) [22], and also by the Colombian Air Force to obtain detailed maps of the runways after UAV surveys to evaluate risk management in face of an expected increase of their operations in Antarctica, as reported by Tabares (2021) [70]. The construction of basemaps in five sub-antarctic islands along the South Sandwich Arc through UAV surveys was a great help for geological interpretation related to volcanic activity and gas emissions to Liu et al. (2021) [71]. Kuznetsova et al. (2021) [72] developed UAV surveys in the Larsemann Hills area to map the boundaries of lakes to help identifying the factors that determine the formation of water inflow to the lakes. Surveys with several UAVs and sensors with multiple environmental goals were developed by Tovar-Sánchez et al. [73] in Deception Island (South Shetlands). This team used several cameras (visible, multispectral and thermal) to build highly detailed ecological maps, to detect anomalous thermal zones, to identify wildlife and to build 3D models of complex geological formations. They also coupled a water sampling device together with a multiparametric instrument (for measuring ancillary parameters) to a multi-rotor UAV for in-situ water collection of inaccessible or protected areas. The chemical study of ice-covered ponds is important, as to understand how climate change is impacting on their characteristics. The identification of the ponds can be guided by UAV surveys which can provide their description and of the surroundings with detailed images and elevation maps, as shown by Faucher et al. (2021) [74]. In another monitoring procedure, Chen et al. (2021) [75] compared aerial photos with current UAV surveys to quantify the retreat of about 12 m of the shoreline in 30 years  in Inexpressible Island in the Ross Sea, and how it is impacting wildlife, by identifying the change of location of Adélie penguin colonies in the island.

Geophysics
Magnetic anomalies: Aeromagnetic surveys with UAV were developed for the first time in Antarctica in the South Shetlands, more specifically in King George, Livingston and Deception Islands by a team of Japanese institutions using their own UAVs (described in Section 4.4.1). The description of the surveys is provided in detail in the areas of interest showing, for instance, the flight plans and trajectories followed, some mapping results and even the cost associated to a mission, as described by Funaki et al. (2014) [77]. Some surveys were developed relatively far away from the launching and control location, namely the one in Deception Island, where the launch and landing of the UAV took place about 40 km away in Hurd Peninsula in Livingston Island like reported by Funaki et al. ( , 2014 [76,77]. The magnetic data acquired in this aerial survey was integrated in Catalán et al. (2014) [78] with the one obtained from several magnetic marine surveys around the island and also in the inner bay to provide a more complete evaluation of the evolution of Deception Island volcano.

Algorithms
Image processing: Some algorithm development for post-processing the segmentation outputs of several methods through the split and merge of segments was also achieved. Antarctic images are used, among others, to provide a larger testing about the more correct delineation of the homogeneous regions of the UAV image mosaics by Acuña et al. (2016) [23]. The Antarctic dataset used in this testing was obtained in the McMurdo Dry Valleys [34].

Ice and Snow
The broad topic related to ice and snow is constituted by 45 publications, references  , whose subcategories and specific topics, shown in Table 7, refer to the study of glaciers and ice sheets (34 papers), sea-ice (6 papers) and snow features (4 papers). Table 7. Ice and snow applications using UAV in Antarctica (45 papers).

Main Topic Specific Topic References
Glacier ice ( [79], which were used for topographic modelling as described by Bliakharskii and Florinsky (2018) [80]. The assessment of opportunities in using UAV surveys for topographic modelling of ice-sheets was developed by Bliakharskii et al. (2019) [81] based on the data of the previous ice-sheet surfaces publications. A very interesting and sound study on subglacial topography and ice thickness models of the eight largest ice caps of the Argentine Islands is developed by Karušs et al. (2019) [82] nicely integrating ground data with a Ground Penetrating Radar (GPR) in a sampling grid, and aerial data by UAV of the whole islands to get the DEM and image mosaics, with some operational details shown in Lamsters et al. (2019) [83]. In order to help evaluating the interaction of a glacier with the adjacent ma  [88] along the route from the coast to Taishan station in a Chinese National Antarctic Research Expedition (CHINARE), using coordinated multi-sensor observations and in which UAV surveys allowed building elevation models of centimetre resolution.
Glaciers: The assessment of the changes in glacier margins in a specially protected area (ASPA-128) of King George Island was obtained by Pudełko et al. (2018) [89] for a period of four decades through multiple satellite and aerial imagery, which were calibrated with the help of higher resolution datasets obtained after recent UAV surveys. The identification of glacial outflow zones and meltwater turbidity, as to determine their impact on the ecosystem, was obtained through UAV surveys with a multispectral camera in four glaciers in King George Island by Wójcik et al. (2019) [90], which allowed identifying local features (glacial discharge, plume shapes and colours) practically unnoticed in satellite datasets. Wójcik-Długoborska and Bialik (2021) [91], went further in the same topic of research and analysed in much detail the effect of shadows caused by glaciers on the spectral characteristics of meltwater measured in UAV and satellite multispectral images. The monitoring of glacier fronts is performed by Marusazh et al. (2019Marusazh et al. ( , 2020 [92,93] in two of the Argentine Islands (Galindez and Winter). These authors have integrated ground measurements (TLS and photos) with UAV surveys to build a finer 3D cloud of points to better represent the glaciers and detect more accurately their volumetric changes in recent consecutive years. The surface measurements of water quality parameters near coves adjacent to glaciers, as to understand glacial meltwater impacts on marine environments, were developed by Osińska et al. (2021) [94] after the different colours of meltwater plumes provided by UAV surveys in King George Island. The quality of DEM products of glacier surfaces built after UAV surveys is evaluated by Alvarez et al. (2021) [95] by comparison with ground data in Livingston Island, South Shetlands.
Subsidence: A large subsidence event that occurred in 2017 in the Dålk glacier, East Antarctica is reported by Popov et al. (2017b) [96] with highly detailed image mosaics and DEMs obtained after UAV surveys just immediately and some weeks later after the event. The detailed analysis and comparison with pre-event data by Florinsky et al. (2019) [97] led them to conclude that ice-surface hydrological processes were able to cause rapid and deep subsidence of large areas in glaciers. The same glacier and event was also analysed by Zhang et al. (2019) [98], more focused in obtaining high quality data after UAV surveys than in investigating the causes triggering the catastrophic event. The same group in another study lead by Li et al. (2020) [99], incorporated elevation data obtained after UAV surveys with LiDAR (Light Detection and Ranging) to improve the characterisation of the evolution of Dålk glacier. Additional details on the monitoring trough multiple annual surveys with UAV of the same glacier, in a Russian and Chinese collaboration, are reported in Skrypitsyna et al. (2021) [100].
Crevasses: Snow-covered crevasses can be detected using very high resolution models built after UAV surveys as validated in the field by Florinsky and Bliakharskii (2018, 2019) [101,102]. The exploitation of textural features of the DEMs through image processing techniques allowed Bliakharskii et al. (2020) [103] and Ishalina et al. (2020) [104] to make crevasse identifications more objective and consequently to improve the detection limit (up to 1 m width) and also to improve the detection rates. This texture based approach was compared to local morphometric features derived from the DEMs by Ishalina et al. (2021) [105], which conclude that both techniques are very useful to detect crevasses and complement each other.
Mapping: The identification and characterisation of sectors of the Antarctic ice-sheet not covered with snow, named as blue ice areas, were obtained through multiple remote and in-situ observations as investigated by Markov et al. (2019) [106]. In particular, the UAV surveys played an important role in creating detailed mapping for local specific analysis. The verification of a technique to properly estimate the albedo of snow surfaces after photogrammetric data and exposure parameters obtained in UAV surveys images is discussed by Zhuravskiy et al. (2019Zhuravskiy et al. ( , 2020 [107,108], detailing their advantages and limitations. To better characterise the seasonal outburst floods on lakes in Broknes Peninsula, Larsemann Hills, Grigoreva et al. (2021) [109] surveyed the structure of snow-ice dams with GPR and UAV.
Thickness: To obtain ice-sheet bed topography and their thickness, radar signals of high-sensitivity and low frequency with 2D aperture synthesis are used. But if the regions of interest correspond to glaciers of a few km in width and the resolution needed is of few hundreds of meters, their survey by manned aircraft is nearly impossible. Leuschen et al. (2014) [110] developed and tested in Antarctica an aerial system with a compact lightweight radar, which demonstrated its potential to collect data over fast-flowing glaciers. The ice thickness obtained by Bello et al. (2020) [111] with a GPR in a glacier in King George Island is accompanied by UAV surveys to build detailed basemaps of the area of interest. A review of the representative results for ice and snow thicknesses obtained with the UAV platforms and radar sensors developed by the Center for Remote Sensing of Ice Sheets (CReSIS), University of Kansas, in their surveys in Antarctica (and in Greenland), also updating recent system advancements and future platforms under development, is comprehensibly described by Arnold et al. (2020) [112].

Sea-Ice
Topography: The detailed 3D mapping of sea ice, below and above, has been obtained with Autonomous Underwater Vehicles (AUVs) and Terrestrial Laser Scanning (TLS), but due to the limitations of TLS in covering large areas as the AUV, Williams et al. (2018) [113] introduced successfully UAVs to conduct photogrammetric surveys to obtain DEMs of the sea-ice surface at the same time as the AUV missions were taking place below. To test the ability of Structure-from-Motion techniques to represent adequately fast-ice surfaces, Li et al. (2019) [114] developed a series of field tests in Prydz Bay, East Antarctica, in which they verified the advantage of making the surveys with low solar illumination angles, as the shadows cast on the surface enhance its details and provide additional tie-points to obtain better mosaics and DEMs.
Icebergs: UAVs surveys were first reported by McGill et al. (2011) [115] to identify and tag free-drifting icebergs. The UAVs launched after a ship in the Southern Ocean allowed observing in detail the margins and surfaces of icebergs and also dropping GPS tracking tags on their top to provide a track record of the iceberg location for many months. The iceberg freeboard, which is critical to estimate its volume, was obtained in sea-ice with a shadow-height novel approach after satellite imagery by Guan et al. (2021) [116], which used very-high resolution models of the icebergs built after UAV surveys to validate the precision of results.
Pancake-ice: As to measure sea-ice features, Williams et al. (2016) [117] developed a pilot study with a pair of off-the-shelf UAVs launched from the icebreaker Nathaniel B. Palmer. The team was able to establish the operational conditions to rapidly deploy the UAVs without interfering with the primary scientific objectives of the cruise. In addition, although the UAVs have experienced poor GPS performances, the team surveyed pancake ice fields and processed the image datasets to segment the pancakes and build size distribution curves.
Sea-ice production: In order to better evaluate changes in thickness and production of sea-ice in Ross Sea a large multidisciplinary team used a set of manned and autonomous platforms to study the coupled air-ice-ocean biogeochemical interactions during a field campaign in the autumn and to relate them to spring conditions, as reported by Ackley et al. (2020) [118]. UAVs based meteorological profiles of the atmospheric boundary layer were obtained simultaneously with ship-based observations of the atmospheric and oceanic heat and momentum balance at the surface as to better understand the effects of wind/wave interactions on sea-ice growth and thickness evolution.  [120]. The synthesis of previous activities with many additional details is presented by Tan et al. (2020) [121], describing the design, development and field trials of their own UAV-mounted snow radar for measuring snow depth over sea-ice. The extent of snow patches was delineated after image mosaics built after UAV surveys by Hrbáček et al. (2021) [122] to assess the role of ephemeral snow cover on ground thermal regime and active layer thickness in ground temperature measurement profiles on a CALM site in James Ross Island, Eastern Antarctic Peninsula. The evaluation of spatial-temporal variability in snow cover was performed by Tarca et al. (2022) [123], which use a local time lapse camera together with a very high resolution orthomosaic and a DEM derived from UAV surveys for identifying how snow cover changes with vegetated areas and the microtopography.

Fauna
The use of UAVs in Antarctic fauna research is reported in 39 publications, references , which have been increasing consistently over the years in the diversity of contents addressed ( Table 8). The majority of the studies focus on counting animals (22 papers), namely penguins, seals, whales and flying birds. Other studies, in smaller number, are dedicated to the morphometric characterisation of seals and whales (5 papers) and to mapping penguin stains in penguin rookeries (1 paper). The interaction with animals, namely for the evaluation of the disturbance the UAVs may cause during the surveys is a major concern when close to penguins, seals and flying birds as well as in analysing the social behaviour of seals and whales (11 papers in total). Table 8. Fauna applications using UAVs in Antarctica (39 papers).

Main Topic Specific Topic References
Counting (

Counting Individuals
Penguins: The counting of penguins is mainly performed on surveys performed over rookeries, being reported in 14 publications. This procedure was first described by Gardner et al. (2011) [124] after surveys in Cape Shirreff in Livingston Island in 2011, detailing the operational aspects required to obtain imagery with adequate quality and also the minimum height to fly the multi-rotor UAV without disturbing the penguins. Similar surveys were developed in several areas and colonies of King George Island with VLOS flights with a fixed-wing system in 2014/15, being the counting of penguins compared to ground measurements, as reported by Zmarz et al. (2015) [125]. The demonstration that UAV-derived counts of colony nesting birds is more precise than traditional ground counts are presented by Hodgson et al. (2016) [126], which propose a method to achieve data compatibility. A multi-modal survey, making the counting directly on the ground and through the analysis of UAV imagery with automated methods on the small Danger Islands (Northwest of the AP), allowed Borowicks et al. (2018) [127] to conclude that these areas have avoided the declines documented in the Western AP and therefore considered to be an important seabird hotspot. The counting and discrimination between Adélie and  [131] in the 2019-2020 summer with four multi-rotor UAVs operating simultaneously. They used a multirobot path-planning method, which allowed covering more than 2 km 2 in 3 h, incomparably quicker than the 2 days normally taken to survey the same area with only one single UAV, normally subject to adequate weather windows. The counting from UAVs surveys are contributing for the global population assessment of Chinstrap penguins together with satellite imagery and ground counting, as developed by Strycker et al. (2020) [132]. A similar procedure is followed by Herman et al. (2020) [133], which compiled the results of their UAV surveys with all census data available to estimate the current global abundance and distribution of Gentoo penguins. Another example on how the counting from UAV surveys is being routinely incorporated in long term monitoring of penguin abundances at the regional scale is reported by Strycker et al. (2021) [134] for Elephant Island. The more frequent surveying and the sheer increase of the amount of data, has lead Liu et al. (2020) [135] to develop an efficient pipeline for counting penguins automatically with a deep learning model, distinguishing penguins on their nests during incubation from penguins with their chicks on the nests after incubation. The careful validation of the counting of penguins from UAV surveys was developed by Dunn et al. (2021) [136] with ground counts collected simultaneously to the aerial flights, identifying the resolution required to discriminate contiguously breeding Chinstrap and Adélie penguins, which were very similar when observed from overhead.
Seals: The basis for an operational implementation of UAV-based detection of individuals is provided by Mustafa et al. (2019) [137], which evaluated quantitatively the ability to distinguish between five different species of seals, but also of seven flying seabirds species, as a function of the spatial resolution of the image datasets. A breeding elephant seal colony in King George Island was monitored with UAV surveys, together with ground cameras and field observations, for about two months by Fudala and Bialik (2020) [138], which allowed deriving population counts and respective body size parameters, which were used to determine the age and sex of individuals. Elephant seals were also identified in the beaches   [142] using the image mosaics built after UAV surveys. These authors also go a step further by exploiting the detailed DEM built to describe fine-scale nest-site selection in relation to topography and better understand the influence of landscape structure on animal population dynamics. Antarctic shags were also counted by Pfeifer et al. (2021) [143] on Nelson Island (but on a different region of the previous authors) and western King George Island after several UAV surveys. These products allowed identifying the distinctive features of shag colonies from those of penguin colonies, since those species often overlap spatially, to guide future survey campaigns. The assessment of the number of active nests and chicks of giant petrels was carefully and successfully developed by Fudala and Bialik (2022) [144] in ASMA 1 in King George Island, which also enhanced the less invasive procedure of the UAV surveys.

Morphometrics
Seals: Morphometrics of pinnipeds, namely length and width of leopard seals lying on the beaches were obtained by Goebel et al. (2015) [145] after UAV flights in Cape Shirreff in Livingston Island, where they also identify fur seals and count and distinguish individually Chinstrap and Gentoo penguins. In Krause et al. (2017) [146], with some of the authors of the previous paper, an adaptable photogrammetric approach for estimating the mass and body condition of pinnipeds using UAV surveys is proposed, which is tested with high accuracy on leopard seals of known body size and mass. Whales

Interaction
Disturbance: The effect of operating UAVs close to wildlife, specially the disturbance that may be prompted by the aerial equipment to penguins, seals and flying birds, has been a major concern of teams working with these tools, and also subject of several studies.  [154], which verified that the behavioural and physiologic responses of sub-Antarctic seabirds to UAV flights are not the same for albatrosses, petrels or penguins. A report on animal wildlife response to close UAV operation is summarised by Mustafa et al. (2018) [155], evaluating the published scientific literature, but also the expert opinion of action groups, personal communications and yet unpublished works. The assessment of the reactions to a UAV was also performed with Weddell seals during the breeding season, as detailed by Laborie et al. (2021) [156] after several flights in Dumont D'Urville, East Antarctica, which verified a low impact for flight at more than 25 m above the ground. Experiments conducted by   [157] show that the response of penguins and seals were significantly more intense with traditional ground surveys than with UAV overflights, which also suggest the best practices for UAV surveys. The generic analysis of the responses of Emperor penguins to UAV surveys and the comparisons of the effects of human approach are presented by Rümmler et al. (2021a) [158], which are detailed according to the type of UAV, overflight height and season of the year on the behaviour of Emperor penguin adults and chicks in Rümmler et al. (2021b) [159].
Behaviour: Video and still imagery obtained in UAV surveys have been used by Johnston (2019) [160] to assess the bubble-net feeding behaviour of humpback whales in the western Antarctic Peninsula. In a close topic, UAVs are used by Bouchard et al. (2019) [161] to observe the behaviour responses of humpback wales to food-related chemical stimuli, being the experiments released into the water along the Antarctic Peninsula to evaluate the involvement of chemoreception in feeding ecology.

Technology
The development of technology to be used in field activities in the harsh Antarctic environment requires dedicated specifications, as described in 27 publications, references [18][19][20]. The subcategories found on this topic are synthesised in Table 9, with most of the contributions focused on the design and development of platforms (10 papers) and sensors (5 papers). The testing of the equipment is presented in 11 publications, encompassing simulations and field trials, control and navigation evaluations and the assessment of the fatigue of the equipment during its lifetime. Table 9. Technology of UAVs in Antarctica (27 papers).

Main Topic Specific Topic References
Platforms ( This led to the design of small UAVs, whose main requirements for polar regions are presented by Chen et al. (2009) [162]. These authors also report the development and integration of the different components of the systems, together with the first field trials in Antarctica, developed in the neighbourhood of Zhongshan and Progress stations in late 2007. The creation of an integrated method for the early-phase design of robust systems is presented by Agte et al. (2012) [163], which demonstrate its validity on the design of a long-endurance UAV for surveys in Antarctic environments. The systems must be designed to face uncertain events and failures, being these issues presented with high detail, using concurrent manipulation of design and failure rate variables combined with integrated performance and probabilistic analysis. Another project devoted to the conceptual design of a specialised UAV to operate in windy and turbulent environments of Antarctica is envisaged by Goraj (2014) [164], presenting the details on the design of the platform, selection of external layout, control devices, structural design and on-board equipment. The design of a small fixed-wing UAV named PW-ZOOM, which had been successfully used in many missions, is described by Goetzendorf-Grabowski and   [165], not only showing how they have designed the system according to the field objectives to achieve, but also provide many details about their development and the initial field tests in Antarctica in the summer of 2014-2015. The same team from the Warsaw University of Technology, continued designing novel UAV models for usage in Antarctica of tailless type (MONICA-1 and MONICA-2), which are more compact and portable, as presented with many details in Rodzewicz et al. (2018) [166]; the field trials in Antarctica near Arctowski station in King George Island allowed the team to check the components performing well and also those requiring improvement in each UAV.
Development: A group of Japanese institutions initiated a pioneer project designated Ant-plane to build and develop UAVs to be specifically used in Antarctica. The set of five models Ant-Plane (1 to 5) are presented in detail in Funaki et al. (2006) [18], Higashino et al. (2007) [167] and Funaki et al. (2008) [168] with schematic diagrams and design drawings and whose generic specifications allow understanding the type of surveys that can be developed in Antarctica. A similar early project concerns a small UAV designed, developed and tested by a team of the University of Beijing aiming to be used in polar environments, as described by Liang et al. (2008) [169], with a brief description of the control system, the tests developed in laboratory simulating the conditions of extreme environments and also the preliminary flight trials in Antarctica. The development of a flight control system that improves control, stability, and resistance of a UAV is described by Garcia and Keshmiri (2013) [170], whose modelling performance was verified with actual UAV flight test data.

Sensors
Design and development: A radar sensor to fly on the fixed-wing Meridian UAV, under development by a team from the University of Kansas, was presented by Blake et al. (2008) [171]. A distributed architecture was proposed, placing the transmitter/receivers along the wings of the UAV to satisfy the mass and volume constrains of the platform. The same team presented two radar sensors to fly with UAVs in polar regions, as described by Lewis et al. (2009) [172]. The accumulator radar is intended to measure internal ice layers up to 100 m depth, while the altimeter radar measures surface relief and near-surface internal layers (up to 10 m). The assemblage of a set of sensors designated CULPIS (The Colorado University LIDAR Profilometer and Imaging System) to fly on UAVs to map surface elevation and topography is developed by Crocker et al. (2012) [173]. The sensors consist of a Light Detecting and Ranging (LiDAR) instrument, an Inertial Measurement Unit (IMU), a Global Positioning System (GPS) module and digital still and video cameras, integrated in four different UAVs. The package was flown in the Aerosonde platform in Terra Nova Bay in late 2009 to measure sea-ice topography and ocean waves. A surveying system constituted by two types of radar was developed by Uribe et al. (2014) [174] to measure ice thickness and snow accumulation. This express system of low power consumption, weight, volume and cost was first tested in Antarctica in late 2010 with a tractor traverse but envisaged to be later incorporated in a UAV. Both radars proved to be adequate to detect subglacial topography, as well as measure multiple internal snow layers and the snow/ice boundary layer. In order to establish the design parameters of a radar system to measure snow depth and permitivitty for UAV mounting, Tan et al. (2017) [175] have undertaken several field experiments in Antarctica in the summer of 2016.

Testing
Simulations and field trials: The testing of platforms is a crucial procedure during the development phase for improving their design before the regular utilisation in field surveys (Lan et al. (2012) [176]). A synthesis of UAV surveys developed in Antarctica with different systems and in distinct campaigns by a team of Japanese institutions is presented in   [177] and by   [19]. These valuable contributions, besides the brief description of the UAVs developed and the application topics addressed, also report on the operational experiences and the lessons learned from development in Antarctica. Modelling aerodynamics is a fundamental step in the design and development of a UAV as Smith et al. (2015) [178] demonstrate with the Meridian platform developed by the University of Kansas, and which has flown intensively in both polar regions. A series of flight trials launched from the ice patrol ship HMS Protector to assist with navigating were performed along the South Shetlands and Western Antarctica Peninsula as reported by Keane et al. (2017) [179]. They allowed checking in detail navigation procedures with pre-planned autopilot control and the quality of video footage, together with the difficulties for the recovery of a fixed-wing UAV in Antarctic sea conditions. An overview of the set of radar instruments that have been developed by the University of Kansas to fly in occupied and unoccupied aircrafts is presented by Rodriguez- Morales et al. (2017) [180]. They also report the tests developed with the radar sensors in both polar regions to estimate several parameters, namely, ice thickness, ice surface and bedrock topography, snow cover thickness on sea ice and also the annual accumulation of snow. Some additional tests are also envisaged by Rodzewicz et al. (2017) [181], which analyse the deviations of the optical axis of the photo-camera during the surveys. These are sensitive features to be assessed, specially if the main requirement is to obtain photogrammetric products with high quality. The development of a novel UAV based on previous polar experience of the University of Kansas team is presented by Mckinnis et al. (2020) [182]. It led them to develop a novel design of a platform, more adequate to deal with the atmospheric conditions of the polar regions, after dynamic modelling and flight-test validations. The use of small and low-cost UAVs to produce profiles of atmospheric parameters of lower boundary layers of the atmosphere was assessed in detail by Inoue and Sato (2022) [183]. They have developed a radiation shield to protect the meteorological sensors from the UAV operation, being the equipment successfully tested during winter in northern Japan, in environmental conditions similar to those of Antarctica, delivering quality measures equivalent to those of radiosonde observations.
Control and navigation: The control and navigation procedures of UAVs in the extreme environments of Antarctica were a major concern in the early days. Lei et al. (2011) [184] proposed a novel composite control method to better resist wind disturbance and keep a good tracking performance which, after lab simulations and posterior flight tests in Antarctica, showed an excellent control of the system and its ability to develop stable trajectories under different environmental conditions in a polar region. In addition, the UAV dynamic properties and the accuracy of the flight trajectory played a crucial role in the effectiveness of photogrammetric surveys. This is a major concern of Glowacki et al. (2015) [185], which validated the proper integration of the dynamic systems and the autopilot of the UAV PW-ZOOM they have designed and developed, during the execution of the aerial surveys in Antarctica by the end of 2014 under different wind and turbulence conditions.
Fatigue evaluation: The extreme conditions that UAVs are subject to in the Antarctic environment are reflected in their lifetime. The analysis of the flight-logs and the parameters collected (i.e., wind speeds, air temperatures, among others) is used to assess the fatigue loads during the missions. It is a procedure seldom performed (or at least reported), but that was addressed by Rodzewicks and Glowacki (2020) [20] on the fixed-wing platform PW-ZOOM after tens of surveys in Antarctica. This is an important procedure to better control the lifetime of the UAVs under operation in extreme environments but also to improve the design and development of new platforms.

Main Topic Specific Topic References
Measurements ( [186][187][188]. The accurate calibration of the sensors and the validation of the measurements were developed in detail and, in particular, the data obtained in several low-height flights (below 135 m above ground level), compared very well with those obtained with tower and sodar sensors. Prior to the development of the first UAV surveys in Terra Nova Bay in 2009, Knuth et al. (2011) [189] have analysed its climate in the previous 15 years to get a clear understanding of the local flow regimes and atmospheric conditions and better prepare the field campaign. This analysis, based on near-surface winds, air-temperature and cyclone activity data collected with automatic weather stations and satellite observations, allowed detecting uncharacteristic flow patterns over the region, which would be later very useful for Knuth et al. (2013) [190] when planning the missions. Obtaining temperature profiles of the atmosphere (up to 1300 m) with a small UAV (SUMO) in two opposite seasons (months of January and September) and in two locations, allowed Cassano et al. [191] to identify "the variety of boundary layer temperatures ranging from deep, well-mixed conditions to strong, shallow inversions". In addition, the repeat of successive flights in the same location allowed to observe rapid changes in the structure of the boundary layer. The combined use of two types of UAV systems, fixed-wing for higher altitudes and multi-rotor quadcopter for the lowest 100 m above the surface, allowed obtaining complementary highly resolved profiles when compared to commonly used and tested systems (radiosonde and tether sonde).
A winter campaign developed aboard RV Polarstern measuring temperature, humidity and wind in tens of flights above sea-ice in the Weddell Sea showed a strongly varying ABL structure [192]. These detailed observations, besides supplementing the regular standard meteorological measurements, allowed verifying that the changes on the ABL structure can range from slightly unstable temperature stratification near the surface to strong surfacebased temperature inversions. To complement the tower measurements of the ABL and improve the modelling of the ABL over Antarctic ice-shelves, UAV surveys were developed in the Ross Ice Shelf during the summer by Wille et al. (2017) [193]. The novel and more detailed measurements performed in flights up to 800 m height, showed the presence of a larger than expected dry bias in the Antarctic Mesoscale Prediction System (AMPS). The detection of the bias on wind speed and dry-relative humidity, throughout the depth of the ABL, is an important result to help improving high-resolution forecasts. In particular, it can improve the AMPS relative humidity product and consequent cloud forecasts over the ice, with an important reduction of the amount of costly aborted aircraft missions over the Antarctic continent.
Although the potential of using UAVs for ABL studies in the Antarctic environment has been demonstrated in the previous publications, Lampert et al. (2020) [194] reinforce it with additional and more detailed results after surveys with three different UAVs, where their flexibility was particularly enhanced, namely, to work permanently under low temperatures (−20 • C) and close to the surface (heights below 100 m), an important factor to study the very shallow polar ABL.
Obtaining additional atmospheric observations for improving weather forecasts in the Southern Ocean is a major concern of Sun et al. (2020) [195]. The UAV surveys performed during winter in the Weddell Sea from the RV Polarstern have improved the analyses of air temperature, wind speed, and humidity. Although concluding that there still is more benefit from the assimilation of radiosonde data than from UAV data, it is very likely that this importance will change rapidly when even lower-cost UAVs will be able to measure profiles throughout the troposphere. UAVs are retrievable and reusable, are better in portability and mobility, and both vertical and horizontal profiles can be obtained in a controlled way and vertical profiles are truly vertical.
The flight strategy employed during six Antarctic missions with the small UAV SUMO, the data processing and the quality control applied to the data are synthesised by Cassano et al. (2021) [196], showing examples of the features measured and the data availability. The compilation of cloud and aerosol data measured during a voyage in 2018 in the Southern Ocean are presented by Kremser et al. (2021) [197], describing the use of UAV, together with other systems, to conduct atmospheric measurements.

Air-Surface Coupling
The influence of the type of surface on the ABL has been evaluated with detail over polynya, bare ground and sea-ice with support from UAV surveys.
Polynya: Polynya are areas of nearly ice-free water surrounded by sea ice and land, whose influence on the above atmospheric layer was evaluated in Terra Nova Bay by Cassano et al. (2010) [198] and Knuth et al. (2014) [199]. The intense air-sea coupling over these areas was monitored using fixed-wing UAVs of the atmospheric state (temperature, humidity, pressure and winds) during the austral winter of 2009. The sensitivity of the set of 3D measurements collected along the flight trajectories between 150 and 3000 m altitude allowed estimating accurately the heat-fluxes on the ABL, providing also specific contributions to improve future campaigns. The evaluation of the ABL and surface conditions during katabatic wind events were performed by Wenta and Cassano (2020) [200] in the Terra Nova Bay polynya using UAV observations coupled with numerical modelling and weather station measurements.
Sea-ice: The same team continued developing similar procedures, but now to evaluate the interactions between air and sea ice. For that purpose, Cassano et al. (2016) [201] developed a field campaign in Terra Nova Bay by the end of winter (September 2012). In addition, the much larger number of flights, contributed to a more comprehensive threedimensional view of the state of the atmosphere (air temperature, humidity, pressure and wind) and the surface skin temperature.
Nunataks: Other surfaces of interest in the coupling with air are nunataks, areas of exposed rock rising above the surrounding glacier ice or ice-sheet surfaces. These rocky areas absorb more solar radiation than the surrounding ice, providing a heterogeneous solar heating of the surface and causing a local destabilisation of the air above them. To better understand these patterns, a fixed-wing UAV was used to take measurements up to 2300 m of altitude above in the in Dronning Maud Land by Stenmark et al. (2014) [202]. This data, complementing the measurements obtained by balloons and ground weather stations, allowed calibrating a model able to simulate temperature profiles and wind patterns on the ABL above bare ground.

Sampling
Aerosols: To improve the sampling of aerosols, Higashino et al. (2014) [203] devised a system composed by a balloon and a UAV. The UAV, which collects the aerosols and also carries meteorological sensors, was suspended on the balloon. The atmosphere measurements and sample collection were performed during the ascent phase till the target altitude is reached, after which the UAV separates from the balloon to return automatically to the home point. This very clever coupling was successfully tested in Antarctica up to a altitude of 8000 m, always retrieving the observation sensors and aerosol samples after each survey, obtaining more measurements in shorter periods of time, and this way reducing the costs involved. This approach is updated with additional details and results by   [204,205].

Others
The use of UAVs in Antarctica is a very recent activity whose legal framework was not included in any previous legislation or regulation. A small set of 5 publications, references [206][207][208][209][210] indicated in Table 11, addresses these issues together with protocols and guidelines to follow during the field surveys and also the results of questionnaires to UAV users on polar regions about global satellite satellite systems (GNSS) or on how UAVs are used in a national polar program. Table 11. Other topics related to the use UAVs in Antarctica (5 papers).

Main Topic Specific Topic References
Legislation ( User surveys (1) GNSS Sheridan (2020) [209] Support to logistics (1) Field expeditions   [210] Legislation: The questions raised about the safety and possible environmental impacts of using UAVs in Antarctica is addressed by Leary (2017) [206], who considered their use for scientific purposes and by touristic activities. The benefits and risks that the use of UAVs pose in Antarctica are presented and based on a comprehensive set of examples linking them to the discussions and the emerging debates within the Antarctic Treaty System after the preparation of discussion documents by some countries. This author also dedicates some attention to analyse the 'The UAS Operator's Handbook', submitted to COMNAP to the ATCM XXXIX held in 2016, noting that although no resolution and therefore no legal effect is achieved, it has been used as guidance by the national Antarctic programmes. This situation is still the same by today.
Guidelines: A protocol was first proposed by Ratcliff et al. (2015) [207], describing the most adequate operational rules to develop successful surveys in penguin colonies without disturbance and also in the processing of the images. Although being developed after surveys on penguin colonies in the Falklands/Malvinas, its content is perfectly suitable for Antarctic surveys, the reason why we decided to also include it in this review. A more complete framework is developed by Harris et al. [208] which evaluate the interaction of UAVs with wildlife to propose a set of comprehensive environmental guidelines about its application in Antarctica. It includes recommendations for the complete surveys procedures, namely, pre-flight preparations, on-site and in-flight protocols, and for post-flight actions and reporting. Although these authors consider that many gaps still exist in understanding the interaction of UAVs with wildlife in general, and not only in Antarctica, they consider that their guidelines could be at the basis of a model to be adapted for use elsewhere in the world.
User surveys: Insights about the choices and performance of Global Navigation Satellite Systems (GNSS) use for drones in polar regions are provided by Sheridan (2020) [209], which compiled and analysed the answers obtained after a survey with researchers using UAVs in the Arctic and Antarctica for scientific research. The survey questions allowed getting a good and detailed picture about the experience in the field, namely about the GNSS used (single or multiple frequency) and the efforts made to augment GNSS signals. Support to logistics: The importance that UAVs are playing to support research and logistics in the frame of the Chinese National Antarctic Research Expedition (CHINARE) is synthesised by   [210]. The support given to science by UAVs is based on several of the publications led by Chinese authors in different topics (terrestrial, glaciology, terrestrial, fauna, atmosphere), which are also analysed in this review. The most novel aspect of this paper is the description of the support to logistics in different phases of the campaigns, namely in safety guarantee (icebreaker navigation, transportation on sea-ice, inland crevasses detection or emergency rescue) but also in construction management (gathering detailed data to help selecting the ideal ice-sheet site for an airfield runaway) and also in education and public outreach activities.

UAV Platforms
Two main types of platforms have been used in surveys the Antarctic, fixed-wing and multi-rotor. Fixed-wing platforms are more used (51.1%) than the multi-rotor (38.9%), although in some publications both types are used (4.2%). Also, only in some cases it was not possible to identify the type of platform used. It is also worth analysing the type of platform by application topic since the predominance is different (Table 12). In the Terrestrial studies the preference is bit a larger for multi-rotor platforms. In the Ice and Snow studies the main option is for fixed-wing UAVs. A larger difference is found on Fauna applications, with multi-rotor being more than the double of the fixed-wing. In Technology almost all developed platforms are fixed-wing type, with only a residual option for multi-rotor. Fixed-wing platforms are always used in the topic Atmosphere, except in a couple of cases where both types are used in complement. The number of manufacturers of UAVs used in Antarctica differs according to the type of platform, being 19 for fixed-wing and 16 for multi-rotor.
The 19 different fixed-wing brands are practically and equally distributed by ready-touse UAVs (or off-the shelf or commercial) and purpose-built UAVs (or customised), with 9 and 10 manufacturers, respectively. The complete picture about the different fixed-wing used is presented in Figure 5, where the most often used are those of Geoscan Ltd. in Russia (16%), and the purpose-built UAV from the Warsaw University of Technology in Poland (15%). The next ones, in order of importance, are UAVs purpose-built by teams lead by universities, some of them incorporating companies also, namely from the Kyushi University in Japan (14%), the Kansas University in the USA (8%), the Beijing University in China (7%), the Bergen University in Norway or the Braunschweig Technical University in Germany (6%). Only the Aerosonde models from the company TEXTRON Systems in USA (7%), are able to meddle in the previous sequence. The picture for the multi-rotor UAV is rather distinct, where the 16 multi-rotor systems correspond to 10 ready-to-use and 6 purpose-built UAV manufacturers ( Figure 6). There is a clear dominance of the DJI equipment from SZ DJI Technology Co., Ltd. in China, which correspond to 57% of the publications with multi-rotor UAV in Antarctica. This may result from the very competitive pricing offered by the company, but also from the large number of models available and tested in Antarctica

Sensors
The main types of sensors carried by UAVs are cameras, in 73.9% of the surveys, which are mainly RGB (65.9%), with marginal use of multispectral (4.5%), hyperspectral (1.7%) and thermal (1.7%) cameras. The majority of the RGB cameras are already incorporated in the UAVs, namely, the DJI platforms (Phantom, Mavic) together with Zenmuse X3 and X5 camera models (in Inspire and Matrice platforms). Several models from Canon (550D, 700D and EOS, in similar proportions) and Sony (mostly DSC-RX1, with few uses of Alpha NEX and SLR) were also frequently used in the surveys. Several other brands of cameras were employed in a smaller number of occasions (MAPIR, Nikon, Olympus, Panasonic). The multispectral cameras carried by UAVs in the Antarctic surveys operated in red, green, blue, red-edge and near-infrared spectral bands and are from the manufacturers Micasense (Red Edge models), Parrot (Sequoia+) and Tetracam Inc. (micro-MCA). For the hyperspectral cameras, there is one single hyperspectral sensor, from Headwall Photonics, with 320 bands in the spectral range 400-1000 nm. It was used in the mapping and health assessment of vegetation [33,42,43]. The thermal cameras were used in scarce surveys, but together with multispectral and RGB sensors, are: the FLIR Photon 320 camera (FLIR Systems, Inc.) carried by a multi-rotor UAV to assess the health status of vegetation [41,44], and the ThermoMAP camera (senseFly) in a classic eBee fixed-wing platform to improve the identification of Adélie penguin individuals [130].
Meteorological sensors (temperature, pressure, humidity and wind) are the second main type of payload with 11.4%, followed by radar sensors used in 5.1% of the cases and magnetometers with a weight of 3.4%. The four main types of meteorological sensors are used in both types of platforms: in fixed-wing UAVs to greater heights, typically of hundreds to thousands of meters and multi-rotor UAVs for smaller heights, typically of tens to a few hundred meters. The diverse radar sensors were developed and applied for different purposes: sound radars to survey glaciers and ice-sheets with large fixed-wing UAVs [110,174], snow radar integrated with multi-rotor UAV to measure snow depth up to 1 m [119][120][121]. As to the magnetometers used in the surveys in the South Shetlands, as payload of the Ant-plane UAVs, were of two types, a three-axis fluxgate system and a magneto-resistant system [77,78,168].
The remaining 6.2% correspond to a varied set of sensors used only once or twice. They refer, for instance, to a LiDAR system (Light Detection and Ranging), being the model used a Velodyne VLP-16, mounted on a DJI Matrice 600 Pro, to make surveys up to 30 min each for ice dolines monitoring [99]. Although there is a broad consensus on the importance of LiDAR data for cryosphere applications [16], their use in UAV surveys in Antarctica is still scarce, probably due to its excessive cost in relation to that of the platform itself. In a distinct topic, a sound meter was used to assess the noise levels emitted by multi-rotor and fixed-wing UAVs, since it is assumed that penguins perceive these aerial platforms mostly by sound [158,159]. Another distinctive application consisted of aerial gas measurements related to volcanic activity obtained with sensors installed in a multi-rotor DJI Matrice 200. These in-situ measurements of gas chemistry, emission rate and carbon isotope composition were sometimes performed beyond visual line of sight along the South Sandwich Arc [71].

Discussion
The identification of the main periods of use of UAVs for science in Antarctica, along with the operational and practical problems faced by the teams in the development of the surveys in the different topics, is necessary to understand their evolution pathways and to identify prospects for topics of interest not yet addressed in Antarctica.

Synthesis
The annual analysis of publications by application reveals an uneven distribution from 2006 to 2010 with few UAVs used in Antarctica and for specific purposes (Figure 7). After 2010, the situation started to change gradually to a more generalised and regular use of these systems across research topics. Initially, the focus was mainly related to the design, development, and testing of technology, both on platforms and sensors, specially in Atmosphere, where customised systems dominated. The development of purpose-built systems was accompanied by growing surveys in Antarctica, boosting after the emergence of small and lightweight UAVs around 2012-2013. In that period, UAVs became out of the box solutions of easy commercial access and more affordable. After 2014, the growth of diversity of applications is remarkable, namely those related to Terrestrial, Ice and Snow and Fauna which in 2020 are the most active fields using UAVs. Atmosphere related studies, and also the first to be developed in the field, have a smaller weight but have kept a regular and constant usage along the last decade. The early designs and the regular technological improvements of UAV platforms and sensors for the harsh polar environments were fundamental for the current stable situation where UAV surveys are regularly used to support scientific activities in Antarctica. Many advances were possible to accomplish in terrestrial topics related to vegetation mapping and characterisation (discriminating main populations, health assessment, fine scale change detections), the generic elevation and surface mapping with unprecedented detail at multiple scales (whole peninsulas and small islands, moraines and stone circles clasts granulometries, ecological maps, anomalous thermal zones, magnetic anomalies). For ice and snow, the topography of glaciers and ice-sheets achieved a detail not seen before, which allowed the detection of subsidence events, the mapping of small crevasses or a better thickness estimation and characterisation of glacier ice. The characterisation of sea ice has also been greatly improved in topographic details, as well as a more detailed description of icebergs and ice pancakes. For snow, the surface and depth characterisation are also much finer. The UAV surveys are having great importance in the fauna topic in the counting of individuals (penguins, seals, flying birds), but also on their morphometric characterisation with an accuracy and quantities not achieved before and, above all, with minimal wildlife disturbance. The atmosphere studies are much enriched with the complementary and detailed measurements provided by the UAV surveys on the ABL, with particular evaluations of different air-surface couplings.

Operational Problems
The Antarctic harsh environment poses important challenges to UAV surveying. However, not all authors describe the operational issues, and the ones providing some information are, in general, not detailed. For this reason we decided to list only the operational problems generically and not presenting a statistical analysis.
Most difficulties reported relate to meteorological conditions before and during the flight surveys, which had frequently to be postponed, delayed or suspended. The main limiting factors are wind speed, rainfall and snowfall. The presence of fog or of very low clouds is also mentioned, although a 'grey sky' with homogeneous illumination conditions is considered to be an advantage for building well-balanced image mosaics.
The possible interference with flying birds during the flights is also a major concern mentioned by several authors, which had sometimes to abort the flights or to move the launch/landing site when relatively close to nests. A good overview about the Antarctic wildlife response to UAVs was presented by Mustafa et al. (2018) [155].
The importance of the quality of Global Navigation Satellite Systems (GNSS) cover is also mentioned, mainly for the development of the UAV flights and also for the collection of ground control points, indicating the difficulties and ways to mitigate them in the development of the Antarctic surveys. Although a complete view about the GNSS used during the surveys is not possible to obtain, as authors seldom indicate it, the most common named choices for navigation and positioning were GPS (Global Positioning System from the United States), Galileo (the European Union GNSS) or GLONASS (Global Navigation Satellite System from Russia), and sometimes a combination of them, which matches the answers given in the survey developed by Sheridan (2020) [209]. No references were found mentioning problems posed by poor GNSS coverage or faulty GPS systems, an issue that was frequently mentioned by teams operating at high latitudes.
The major and common operational problems faced with the UAV platforms and sensors in Antarctica are related to battery-powered units. As reported by some authors, the duration of the surveys was much reduced or not possible at all with temperatures much below 0 • C . Anyhow, nowhere is reported a serious accident or the loss of a UAV in the Antarctic.

Novel Application Topics and Methodological Developments
Although the main thematic areas analysed before are prone to expand and accommodate more developments, there are some new specific topics, and also applications borrowed from the Arctic, that can be also developed in Antarctica with the support of UAVs. Without being exhaustive, we identify the following topics that have potential for development in the Antarctic.
The collection of meteorites in Antarctica is a very successful task developed regularly for several decades with systematic field campaigns [211,212]. The remote identification of meteorites, or at least the creation of hotspots for posterior local inspection, can be greatly helped by UAV surveys also incorporating, besides RGB cameras, some specific sensors (thermal, multispectral). So far, there is no mention in the literature to the systematic use of UAV for looking for meteorites.
The development of GPR surveys has been accompanied by separate aerial UAV surveys of the same area in some projects in the Antarctic to provide, for instance, a more complete assessment of ice volumes and surface topography [82,109,111]. Although the integration of GPR sensors in UAV platforms is already technically available, their use in cryosphere studies is still limited to few surveys in the Arctic, namely to measure snowpack properties [213], and still without references in the Antarctic. The benefits of its use are immediate and evident, namely in clear time efficiencies in the development of the field work compared to traditional ground surveys, as well as clear cost advantages when compared to aircraft manned flights. Accessibility to difficult places by foot (or inaccessible at all), with the obvious advantages of avoiding hazardous environments, will become this way feasible. Furthermore, the development of aerial surveys with precise measurements makes this coupling very attractive for research in Antarctica.
The sampling and collection of physical samples (ice, snow or water, but also soils or rocks, for instance) in distant, inaccessible and difficult access sites can be a major task to be developed with the support of UAV. For water, this is already being accomplished in Antarctica using a sampling device for samples collection and also a small multiparametric probe to measure in-situ ancillary parameters [73]. Since its applicability was currently demonstrated, it is expected that these systems will become frequently used in this kind of tasks.
The capabilities of a UAV to retrieve glacial ice samples was demonstrated in the field by Carlson et al. (2019) [214] in the harsh winter conditions of Greenland. This team developed a multi-rotor prototype based on the off-the-shelf DJI Matrice 600 Pro incorporating a specially designed drill and other sensors (camera, microLiDAR), which clearly opens the way for developing better and more autonomous systems, which can be used for large-scale monitoring of ice in Antarctica.
Although it is common to build image mosaics of centimetre resolution after the aerial surveys, there are still details captured at ground level (at millimetre and sub-millimetre resolutions) [215,216], to identify, for instance, different types of lichens or mosses, that can useful to be integrated in the UAV products.
It is also expected that the processing and analysis of more detailed data will take advantage of current algorithmic trends, namely from machine learning and artificial intelligence. Although machine learning is already being used in publications analysed in the current review, some of them borrowed from other works, there are approaches dealing remotely with Antarctic features through satellite imagery that can be also applied at the UAV scale. They can be used, for instance, to improve the automatic detection of icebergs [217,218], to accurately detect glacier calvin margins [219] or to make a more accurate detection of landfast sea ice [220]. The methods and algorithms developed in the reconstruction of ocean colour data [221], the mapping of supraglacial lakes [222], or the improvements to better resolve bed topography [223] may be also useful for similar data acquired in UAV surveys. The monitoring in infrared images of volcanoes [224] is another spaceborne application that can be transposed to the UAV scale.

Coordination and Data Sharing
Up to now, most UAV applications have been conducted by individual teams, lacking coordination and targeting at specific topics. The increased use of UAVs calls for better international coordination, especially since several Antarctic ecosystems are very sensitive and may be disturbed by an increasing number of overflights and field visits. Open sharing of acquired data and joint survey planning would be very relevant to mitigate environmental impacts, as well as to maximise research outcomes. This would be especially relevant since data gathered for specific scientific goals can also cross-feed other research areas. As an example, the high-quality and resolution of data collected by UAVs can be integrated in an open-access archive to be used as ground truthing of satellite-based data. Such a jointly coordinated effort could be fostered within the Scientific Committee on Antarctic Research, and would bring increased benefits for Antarctic research, as well as to the management of Antarctica, with potential linkages to the Antarctic Treaty System.

Conclusions
The extensive analysis of the publications on applications, methods, technologies and sites associated to UAV-supported research, evidences the increasing relevance of these for data collection in Antarctica. This growth is clear in the increasing number of scientific articles. Three main periods from 2006 to 2021 are identified: (i) 2006 to 2013 is dominated by surveying using in-house developed equipment and shows an average of about 3 papers/year, (ii) 2014 to 2018 coincides with the increased availability of commercial equipment and shows an average of 12 papers/year, (iii) after 2019 is a transition to a mature period with increased expertise and availability of platforms and sensors, and the widespread use of UAVs in most research topics, leading to the publication of 34 papers/year.
Many of the studies assessed were only possible to be conducted with UAV-derived data. For the terrestrial studies, highlights are on the much more detailed and extensive geomorphological mapping, as well as on the more precise mapping and monitoring of vegetation in relatively large areas, including the spatial assessment of health indicators. The identification and characterisation of cryospheric features is greatly improved with detailed 3D data, including subsurface applications. Improved counting and morphometrics of individuals (penguins, seals, flying birds or whales), conducted with little or no disturbance, are a major breakthrough in the fauna studies. UAV atmospheric surveys provide faster data collection and with unraveled versatility, including collecting aerosol samples. The pioneer design and development of novel platforms adapted to the Antarctic environment was crucial for full applicability in harsh environments. Using UAVs for collecting physical samples of ice, snow, water, soils or rocks, at distant or inaccessible areas, is already possible, but the increase of autonomy and robustness will make these systems even more appealing for Antarctic field work.
The evolution of the usage of UAVs in Antarctica since 2006 shows a currently wellestablished practice in many research areas. Most authors recognise its huge potential and use UAVs routinely, being expected an increase in its applications in more and diversified research topics in Antarctica. An internationally coordinated effort for planning and sharing UAV data in Antarctica becomes this way much needed.
Author Contributions: P.P. and G.V. designed the structure of the manuscript. P.P. performed the bibliographic search and organised the survey. P.P. wrote a preliminary version of the text, which was developed and reviewed by PP and G.V. All authors have read and agreed to the published version of the manuscript.