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Published on: November 18, 2022
Snow depth variability in the Northern Hemisphere mountains observed from space
Hans Lievens1,2, Matthias Demuzere3,4, Hans-Peter Marshall5,6
1Department of Earth and Environmental Sciences, KU Leuven, Heverlee, Belgium. hans.lievens@kuleuven.be.
Sentinel-1 satellite data can now map Northern Hemisphere mountain snow depth at 1 km² resolution. This advancement aids in assessing global water resources and climate change impacts on snowpack.
Area of Science:
- Earth Observation
- Hydrology
- Remote Sensing
Background:
- Accurate snow depth data is crucial for managing water resources, especially in Northern Hemisphere mountains where over a billion people depend on snowmelt.
- Current large-scale remote sensing of mountain snow depth remains a significant challenge.
Purpose of the Study:
- To demonstrate the capability of Sentinel-1 satellite data for mapping mountain snow depth across the Northern Hemisphere.
- To provide a foundation for long-term monitoring of snow-water resources and their vulnerability to climate change.
Main Methods:
- Utilized an empirical change detection approach with Sentinel-1 data.
- Mapped snow depth at 1 km² resolution in Northern Hemisphere mountain ranges.
- Validated retrievals using approximately 4000 ground-based measurements and reanalysis data.
Main Results:
- Sentinel-1 successfully mapped snow depth in Northern Hemisphere mountains.
- The data captured spatial variability within and between mountain ranges.
- Inter-annual snow depth differences were accurately represented, as shown by contrasting 2017 and 2018 data in the Sierra Nevada and Alps.
Conclusions:
- Sentinel-1 offers a valuable tool for large-scale snow depth monitoring in mountains.
- The findings support the long-term assessment of mountain snow-water resources under climate change.
- Ensured continuity of Sentinel-1 data until at least 2030 provides a basis for ongoing research and resource management.
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