Remote Sensing of Cryospheric Hydrology and Water Cycle
A special issue of Remote Sensing (ISSN 2072-4292). This special issue belongs to the section "Environmental Remote Sensing".
Deadline for manuscript submissions: 28 February 2026 | Viewed by 11
Special Issue Editors
Interests: arctic hydrology; surface–groundwater exchange; remote sensing
Special Issues, Collections and Topics in MDPI journals
Interests: groundwater modeling; permafrost hydrology; remote sensing
Special Issues, Collections and Topics in MDPI journals
Interests: remote sensing; cold region hydrology; snow; river ice
Special Issues, Collections and Topics in MDPI journals
Special Issue Information
Dear Colleagues,
Advancements in remote sensing technology have transformed the cryosphere into a reliable data source for monitoring its key components, such as glaciers, snow cover, permafrost, and sea ice. Since the 1990s, rapid advances in Earth observation technologies have enabled high-resolution, large-scale, and continuous monitoring of cryospheric dynamics. As a vital source of global freshwater, the cryosphere serves as a critical indicator of climate change. Accelerated warming has triggered significant shifts in its water cycle and underlying surfaces—including precipitation, evaporation, snowfall, and permafrost—further influencing hydrological processes. Accurate monitoring and modeling of these changes are essential for predicting hydrological impacts and ensuring sustainable management of water and environmental resources.
This Special Issue seeks to compile innovative research leveraging remote sensing technologies to monitor, analyze, and model cryospheric hydrology and the water cycle. Contributions may explore the development of novel methodologies, the application of advanced remote sensing techniques, or the integration of multisource and multiscale data to study hydrological processes in cold regions. This topic aligns closely with the journal’s scope, emphasizing remote sensing applications in environmental monitoring and Earth system science.
Suggested themes and article types for submission:
- Advances in remote sensing techniques for cryospheric hydrology and water cycle
- Cryosphere–climate feedback and hydrological responses
- Impacts of cryosphere changes on water resources and ecosystems
- Snowpack distribution, melt, and hydrological impacts
- Permafrost thaw and its hydrological implications
- Modeling of the cryospheric water cycle
Prof. Dr. Ping Wang
Dr. Tianye Wang
Prof. Dr. Hongyi Li
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
- cryospheric hydrology
- permafrost
- snow hydrology
- water cycle
- surface–groundwater interaction
- arctic
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