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Mapping and Monitoring Glacial and Snow Changes through Remote Sensing

A special issue of Remote Sensing (ISSN 2072-4292). This special issue belongs to the section "Remote Sensing in Geology, Geomorphology and Hydrology".

Deadline for manuscript submissions: 15 March 2025 | Viewed by 1030

Special Issue Editors


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Guest Editor
Politecnico di Milano, Department of Civil and Environmental Engineering (DICA)—Geomatics and Geodesy Section, Piazza Leonardo da Vinci 32, 20133 Milan, Italy
Interests: geomatics; UAV photogrammetry; monitoring
Special Issues, Collections and Topics in MDPI journals

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Guest Editor
Research Institute for Geo-Hydrological Protection, Italian National Research Council, Strada delle Cacce, 73, 10135 Torino, Italy
Interests: boundary layer meteorology; image processing; MATLAB; earth observation; deformation monitoring; remote sensing; data integration; glaciology; digital image correlation and tracking; advanced machine learning
Special Issues, Collections and Topics in MDPI journals

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Guest Editor Assistant
Environmental and Infrastructure Engineering, Department of Civil and Environmental Engineering, Politecnico di Milano, Italy
Interests: photogrammetry/SfM; UAV; glaciers; computer vision; digital image correlation; deep learing; multi-temporal monitoring; point clouds; LIDAR

Special Issue Information

Dear Colleagues,

Glaciers and snow cover play a crucial role in freshwater supply, climate regulation, and the Earth's hydrological cycle. However, these frozen water resources are susceptible to the impacts of climate change, leading to significant glacial retreat and alterations in snow patterns. Effective mapping and monitoring of glacial and snow changes are essential for understanding the implications of climate change and informing water management strategies. Remote sensing technology has proven to be a valuable tool in studying and assessing these changes.

The aim of this Special Issue is to explore the advancements in remote sensing techniques for mapping and monitoring glacial and snow changes. We invite submissions that showcase innovative methodologies, techniques, and applications related to remote sensing analysis in the context of glacial and snow monitoring. We welcome research articles, reviews, and case studies that address the following topics:

  • Remote sensing data acquisition and preprocessing techniques for glacial and snow change detection;
  • The development and validation of algorithms and models for mapping and monitoring glacial retreat and snow cover variations;
  • Integration of remote sensing data with in situ measurements or other geospatial information for comprehensive assessments of glacial and snow changes;
  • Advances in multi-temporal monitoring of glacier’s evolution, including (but not limited to) ice mass loss and volume,  glacier extension, and glacier surface velocity variations, using remote sensing techniques;
  • Applications of remote sensing for studying the impacts of climate change on glaciers and snowpacks;
  • Evaluation of the effectiveness of remote sensing in supporting water resource management and climate adaptation strategies.

Prof. Dr. Livio Pinto
Dr. Niccolò Dematteis
Guest Editors

Francesco Ioli
Guest Editor Assistant

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

  • remote sensing
  • glacial change
  • snow cover monitoring
  • climate change
  • water resource management

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Published Papers (1 paper)

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Research

23 pages, 8730 KiB  
Article
Three-Dimensional Surface Motion Displacement Estimation of the Muz Taw Glacier, Sawir Mountains
by Yanqiang Wang, Jun Zhao, Zhongqin Li, Yanjie Yang and Jialiang Liu
Remote Sens. 2024, 16(22), 4326; https://doi.org/10.3390/rs16224326 - 20 Nov 2024
Viewed by 361
Abstract
Research on glacier movement is helpful for comprehensively understanding the laws behind this movement and can also provide a scientific basis for glacier change and analyses of the dynamic mechanisms driving atmospheric circulation and glacier evolution. Sentinel-1 series data were used in this [...] Read more.
Research on glacier movement is helpful for comprehensively understanding the laws behind this movement and can also provide a scientific basis for glacier change and analyses of the dynamic mechanisms driving atmospheric circulation and glacier evolution. Sentinel-1 series data were used in this study to retrieve the three-dimensional (3D) surface motion displacement of the Muz Taw glacier from 22 August 2017, to 17 August 2018. The inversion method of the 3D surface motion displacement of glaciers has been verified by the field measurement data from Urumqi Glacier No. 1. The effects of topographic factors, glacier thickness, and climate factors on the 3D surface displacement of the Muz Taw glacier are discussed in this paper. The results show that, during the study period, the total 3D displacement of the Muz Taw glacier was between 0.52 and 13.19 m, the eastward displacement was 4.27 m, the northward displacement was 4.07 m, and the horizontal displacement was 5.90 m. Areas of high displacement were mainly distributed in the main glacier at altitudes of 3300–3350 and 3450–3600 m. There were significant differences in the total 3D displacement of the Muz Taw glacier in each season. The displacement was larger in summer, followed by spring, and it was similar in autumn and winter. The total 3D displacement during the whole study period and in spring, summer, and autumn fluctuated greatly along the glacier centerline, while the change in winter was relatively gentle. Various factors such as topography, glacier thickness, and climate had different influences on the surface motion displacement of the Muz Taw glacier. Full article
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