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Remote Sensing in Permafrost Region Monitoring

A special issue of Remote Sensing (ISSN 2072-4292). This special issue belongs to the section "Environmental Remote Sensing".

Deadline for manuscript submissions: closed (31 March 2024) | Viewed by 1097

Special Issue Editors


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Guest Editor
Department of Geography and Environment, University of Aberdeen, Aberdeen AB24 3UF, Scotland, UK
Interests: gis; geomorphology; glaciology; geodetic mass balance; glacier elevation change

E-Mail Website
Guest Editor
Department of Geography, Geography and History School, University Complutense of Madrid, 28040 Madrid, Spain
Interests: geomorphology; GIS; cartography; photogrammetry

Special Issue Information

Dear Colleagues,

This Special Issue focuses on the applications of Remote Sensing for research in permafrost and periglacial areas.

Permafrost -the permanently frozen ground- is one of the most prominent elements of high mountain and high latitude environments. The interplay of frozen water, sediment and bedrock and their reaction to environmental changes (daily, seasonal or long-term) creates specific landforms and geomorphological processes. At present, permafrost is being affected by anthropogenic climate change with very varied implications for the environments in which it is found and even faraway areas. Remote sensing techniques, whether they are acquired from ground based, airborne or satellite-borne, can help find, measure and monitor permafrost, periglacial landforms and periglacial landscapes.

Both review papers and contributing papers are welcomed. Contributions should focus on the application of remote sensing techniques to detect, describe, measure or model permafrost and periglacial features, their implications to natural or anthropic systems and the interplay between permafrost and glacial ice or snow. The topics mainly include, but are not limited to, the following aspects:

  • Use of satellite imagery to track the changes in periglacial landforms.
  • Use of satellite imagery to track the changes in snow coverage of periglacial environments.
  • Combined aerial/satellite imagery applied to periglacial landforms.
  • Unmanned Aerial Vehicle applications in periglacial landscapes.
  • Structure from Motion techniques applied to periglacial areas.
  • Airborne or terrestrial laser scanner in periglacial landscapes.
  • Remote sensing of the thermal state of permafrost.
  • Use of Artificial Intelligence over imagery to track and model snow and permafrost evolution.
  • Ground penetrating techniques to find, measure and describe the permafrost layer and its evolution.

Dr. Ramón Pellitero
Dr. Luis Miguel Tanarro García
Guest Editors

Manuscript Submission Information

Manuscripts should be submitted online at www.mdpi.com by registering and logging in to this website. Once you are registered, click here to go to the submission form. Manuscripts can be submitted until the deadline. All submissions that pass pre-check are peer-reviewed. Accepted papers will be published continuously in the journal (as soon as accepted) and will be listed together on the special issue website. Research articles, review articles as well as short communications are invited. For planned papers, a title and short abstract (about 100 words) can be sent to the Editorial Office for announcement on this website.

Submitted manuscripts should not have been published previously, nor be under consideration for publication elsewhere (except conference proceedings papers). All manuscripts are thoroughly refereed through a single-blind peer-review process. A guide for authors and other relevant information for submission of manuscripts is available on the Instructions for Authors page. Remote Sensing is an international peer-reviewed open access semimonthly journal published by MDPI.

Please visit the Instructions for Authors page before submitting a manuscript. The Article Processing Charge (APC) for publication in this open access journal is 2700 CHF (Swiss Francs). Submitted papers should be well formatted and use good English. Authors may use MDPI's English editing service prior to publication or during author revisions.

Keywords

  • permafrost degradation
  • permafrost layer
  • periglacial landforms
  • patterned ground
  • rock glaciers
  • frozen ground
  • snow
  • freeze/thaw
  • unmanned aerial vehicle
  • photogrammetry
  • aerial imagery
  • satellite imagery
  • radar remote sensing
  • optical remote sensing
  • ground penetrating radar
  • electric resistivity
  • digital elevation model (DEM)
  • laser scanner

Published Papers (1 paper)

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Research

19 pages, 10831 KiB  
Article
Rock Glacier Inventory of the Southwestern Pamirs Supported by InSAR Kinematics
by Qiqi Ma and Takashi Oguchi
Remote Sens. 2024, 16(7), 1185; https://doi.org/10.3390/rs16071185 - 28 Mar 2024
Viewed by 625
Abstract
Although rock glaciers (RGs) are prevalent in the southwestern Pamirs, systematic studies on them are scarce. This article introduces the first inventory of RGs in the southwestern Pamirs, situated at the western edge of the High Mountain Asia region. The inventory, established through [...] Read more.
Although rock glaciers (RGs) are prevalent in the southwestern Pamirs, systematic studies on them are scarce. This article introduces the first inventory of RGs in the southwestern Pamirs, situated at the western edge of the High Mountain Asia region. The inventory, established through a combination of Google Earth optical imagery and Interferometric Synthetic Aperture Radar (InSAR) techniques, encompasses details on the locations, geomorphological parameters, and kinematic attributes of RGs. A total of 275 RGs were cataloged in an area of 55.52 km2 from 3620 to 5210 m in altitude. Our inventory shows that most RGs in this region are talus-connected (213 landforms), with the highest frequency facing northeast (23%). The distribution of RGs thins from west to east and is more abundant in higher altitudes. The Shakhdara range to the south hosts a denser and more active population of RGs than the Shughnon range to the north, highlighting the influence of topography and precipitation. Overall, RGs in the southwestern Pamirs exhibit high activity levels, with active RGs predominating (58%). A comparison between active and transitional RGs showed no significant differences in elevation, temperature, and slope. Glacier-connected and glacier forefield-connected RGs demonstrated higher line-of-sight (LOS) velocities than talus-connected and debris-mantled slope-connected RGs, underscoring the significant impact of precipitation and meltwater on their activity. Full article
(This article belongs to the Special Issue Remote Sensing in Permafrost Region Monitoring)
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