Dynamics of Terrestrial Environmental Systems

A special issue of Land (ISSN 2073-445X). This special issue belongs to the section "Land Systems and Global Change".

Deadline for manuscript submissions: 31 May 2025 | Viewed by 6917

Special Issue Editors


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Guest Editor
Department of Solar Energy and Environmental Physics, BIDR, Ben-Gurion University of the Negev, Sede Boqer Campus 8499000, Beer Sheva 84101, Israel
Interests: pattern formation; non-linear dynamics; ecohydrology; aeolian geomorpholgy; spatial ecology
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Guest Editor
School of Geography and Ocean Science, Nanjing University, Nanjing 210023, China
Interests: geomorphology; landscape dynamics; arid zone; quaternary geology; climate change; global environmental change
Special Issues, Collections and Topics in MDPI journals

Special Issue Information

Dear Colleagues,

Various methods, including field studies, controlled laboratory experiments, remote sensing, and mathematical models, enable the investigation of environmental terrestrial systems that include both abiotic and biotic components, showcasing intriguing interactions. These methods have involved collaboration between scientists from different disciplines such as geomorphologists, ecologists, and physicists.  One example is the diverse and intriguing vegetation patterns of water-limited environments. Along the rainfall gradient, these ecosystems exhibit varying patterns, including gaps and fairy circles, stripes, spots, and bare soils. The ability of ecological systems to undergo sudden transformations has long fascinated scientists, challenging conventional expectations of gradual change. These unexpected shifts, known as regime shifts or critical transitions, signify pivotal moments when a system, governed by intricate feedback loops, transitions from one stable state to another through bifurcation or a tipping point.

Even non-living systems, such as bedforms, mountainous topography, and river networks, display dynamic changes across different spatiotemporal scales. For instance, bedforms exhibit multiple scales, featuring small sand ripples of centimeters to larger megaripples spanning meters. The characteristics of these geomorphic systems, influenced by complex physical and chemical processes, provide valuable information about sediment transport, wind regimes, and climate conditions in expansive and often inaccessible regions.

These systems, dynamic and responsive to environmental conditions, play a crucial role in the Anthropocene, where human activities have become the primary geological force. Understanding the dynamics of environmental systems and their feedback is essential for reliable forecasts in human health, welfare, food and water security, and sustainable development.

The primary focus of this Special Issue is to delve into the dynamics of diverse environmental systems, encompassing both abiotic and biotic aspects, and to examine the intricate interplay between these systems driven by climate change and human activities. Exploring the transitions of ecosystems, geomorphologic systems, and other environmental systems, from one stable state to another, becomes crucial in enhancing resilience to climate change.

Moreover, this Special Issue aims to showcase a spectrum of scientific methods employed to study the dynamics of these systems. These methods encompass remote sensing, field experiments, and mathematical modeling, or employ a synergistic combination of various approaches.

In this Special Issue, original research articles and reviews are welcome. Research areas may include (but are not limited to) the following:

Aeolian systems and ecosystems, dryland ecosystems and vegetation patterns, resilience of environmental systems to climate change, self-organization in geomorphological systems, plant–soil hydrological processes, and land surface dynamics. Multi-disciplinary approaches are more than welcome.

Abstract submission deadline:

June 30, 2024

Notification of abstract acceptance:

July 31, 2024

We suggest that, prior to submitting a manuscript, interested authors initially submit a proposed title and an abstract of 200–500 words summarizing their intended contribution. Please send it to the Guest Editors (yiyeh@bgu.ac.il) or to the Land editorial office (land@mdpi.com). Abstracts will be reviewed by the Guest Editors for the purposes of ensuring proper fit within the scope of the Special Issue. Full manuscripts will undergo single-blind peer-review.

We look forward to receiving your contributions.

Prof. Dr. Hezi Yizhaq
Dr. Zhiwei Xu
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. Land is an international peer-reviewed open access monthly 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 2600 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

  • complex environmental system
  • ecosystems
  • climate change
  • remote sensing
  • mathematical modelling
  • drylands
  • tipping points
  • pattern formation
  • aeolian processes
  • geomorphological systems

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Published Papers (3 papers)

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Research

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18 pages, 5863 KiB  
Article
Towards Uncovering Three Decades of LULC in the Brazilian Drylands: Caatinga Biome Dynamics (1985–2019)
by Washington J. S. Franca Rocha, Rodrigo N. Vasconcelos, Diego P. Costa, Soltan Galano Duverger, Jocimara S. B. Lobão, Deorgia T. M. Souza, Stefanie M. Herrmann, Nerivaldo A. Santos, Rafael O. Franca Rocha, Jefferson Ferreira-Ferreira, Mariana Oliveira, Leonardo da Silva Barbosa, Carlos Leandro Cordeiro and Willian M. Aguiar
Land 2024, 13(8), 1250; https://doi.org/10.3390/land13081250 - 9 Aug 2024
Cited by 4 | Viewed by 2697
Abstract
Dryland regions around the world are facing intricate challenges due to climate change and human activities. The Caatinga biome in Brazil, an exceptional dryland ecosystem covering approximately 86.3 million hectares, is particularly impacted by human influence. We conducted an extensive study analyzing changes [...] Read more.
Dryland regions around the world are facing intricate challenges due to climate change and human activities. The Caatinga biome in Brazil, an exceptional dryland ecosystem covering approximately 86.3 million hectares, is particularly impacted by human influence. We conducted an extensive study analyzing changes in land use and land cover within the Caatinga region over a span of 35 years, from 1985 to 2019. This study leverages collective knowledge and collaborative effort with the MapBiomas project to provide valuable insights into the biome’s landscape. It maps eight principal land cover classes using Landsat Collection 1 Tier 1 data normalized to top-of-atmosphere reflectance. All data processing was carried out within the Google Earth Engine platform, and the graphics were generate using R version 3.6.2. This study achieved an impressive 80% global accuracy in the time series of Caatinga land use and land cover (LULC) changes, with allocation and area discrepancies of 11.6% and 8.5%, respectively. The extensive 35-year LULC dataset reveals a substantial 11% reduction in natural vegetation in the Caatinga biome, translating to a loss of 6.57 million hectares. This decline is primarily attributed to the expansion of cattle ranching and agriculture; all types of natural vegetation have experienced decreases, with Savanna Formation (SF) areas declining by 11% and Forest Formation (FF) areas declining by 8%. In contrast, pasturelands expanded by 62% and agricultural land expanded by 284% during this period. With their urgent and significant real-world for informing social, economic, and environmental policy decisions within the Caatinga and other dryland regions globally, these findings underscore the importance and immediacy of our research. Full article
(This article belongs to the Special Issue Dynamics of Terrestrial Environmental Systems)
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19 pages, 3814 KiB  
Article
Quantitative Analysis of Aeolian Sand Provenance: A Comprehensive Analysis in the Otindag Dune Field, Central Inner Mongolia, China
by Yingying Cui, Yali Zhou, Ivan Lizaga, Zhibao Dong, Jin Zhang, Aimin Liang, Ping Lü and Tong Feng
Land 2024, 13(8), 1194; https://doi.org/10.3390/land13081194 - 2 Aug 2024
Cited by 1 | Viewed by 1459
Abstract
The identification and quantification of aeolian sand contributions are essential for understanding the formation of dune fields and mechanisms of modern surface processes. In the present study, we take aeolian sand in the Otindag dune field (hereafter, often referred to as, simply, Otindag) [...] Read more.
The identification and quantification of aeolian sand contributions are essential for understanding the formation of dune fields and mechanisms of modern surface processes. In the present study, we take aeolian sand in the Otindag dune field (hereafter, often referred to as, simply, Otindag) as the research object. The dune field’s immediate source is quantitatively identified based on heavy minerals and the Conservativeness Index (CI), Consensus Ranking (CR), and the Consistent Tracer Selection (CTS) method. The primary source area of the aeolian sand was found to be from the northwestern, upwind area of the Otindag (59 ± 14%), followed by the Yinshan Mountain (17 ± 10%) and the lake basin (23 ± 12%). The proposed sediment transport model elucidates that sediments from the upwind of the Otindag are directly transported from the northwest to the Otindag, where they are deposited. Materials from the southern Yinshan Mountains are carried by rivers to the southern edge of the Otindag, where they are subsequently transported by wind and ultimately deposited. The lake deposits within the Otindag also contribute to the aeolian sand supply under the influence of wind. This study demonstrates that the fingerprinting techniques of CI, CR, and CTS serve as successful strategies for conducting quantitative provenance research in dune fields. Full article
(This article belongs to the Special Issue Dynamics of Terrestrial Environmental Systems)
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Review

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13 pages, 1824 KiB  
Review
Environmental Studies Based on Lake Sediment Records in China: A Review
by Minqiao Li, Guoping Tang and Huasheng Huang
Land 2024, 13(5), 637; https://doi.org/10.3390/land13050637 - 8 May 2024
Viewed by 2080
Abstract
Lake sediment records are of great importance for understanding the evolution of watershed environments. Various studies have been carried out to determine the depositional ages of lake sediments and to examine their physical, chemical, and biological characteristics. The aim is to construct the [...] Read more.
Lake sediment records are of great importance for understanding the evolution of watershed environments. Various studies have been carried out to determine the depositional ages of lake sediments and to examine their physical, chemical, and biological characteristics. The aim is to construct the historical vegetation, environment, and climate patterns in Chinese lake watersheds. In this review, we obtained relevant studies on lake sediment records by searching the key word ‘age-depth’ from the following databases: Web of Science and the China National Knowledge Infrastructure (CNKI, the largest Chinese academic database). We analyzed the literature based on its type (published in a Chinese/English journal or as a Master’s/PhD thesis), period of publication, journal (if published in a journal), key authors, study area, dating scale, and main aims. The results suggest that the lakes in the plateau regions are the most popular research topic, typically covering 100–200 years (short-term) and 500–30,000 years (long-term). The literature focuses on a wide range of topics, from past environmental evolution in watersheds to lake ecology, and it provides a solid foundation for a better understanding of the regional climate change and the preservation of lake environments and ecosystems. In the future, the resulting data obtained from environmental reconstructions with lake sediments will need to be integrated with emerging information processing technologies (e.g., artificial intelligence and meta-analysis) to disentangle the complex interplay between the Earth’s surface processes and global climate change; furthermore, strengthening interdisciplinary collaboration will deepen our comprehension of the man-land relationship and promote the sustainable management of lake ecosystems in the context of global climate change. Full article
(This article belongs to the Special Issue Dynamics of Terrestrial Environmental Systems)
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