Snow depth variability in the Northern Hemisphere mountains observed from space

Hans Lievens*, Matthias Demuzere, Hans Peter Marshall, Rolf H. Reichle, Ludovic Brucker, Isis Brangers, Patricia de Rosnay, Marie Dumont, Manuela Girotto, Walter W. Immerzeel, Tobias Jonas, Edward J. Kim, Inka Koch, Christoph Marty, Tuomo Saloranta, Johannes Schöber, Gabrielle J.M. De Lannoy

*Corresponding author for this work

Research output: Contribution to journalArticleAcademicpeer-review

Abstract

Accurate snow depth observations are critical to assess water resources. More than a billion people rely on water from snow, most of which originates in the Northern Hemisphere mountain ranges. Yet, remote sensing observations of mountain snow depth are still lacking at the large scale. Here, we show the ability of Sentinel-1 to map snow depth in the Northern Hemisphere mountains at 1 km² resolution using an empirical change detection approach. An evaluation with measurements from ~4000 sites and reanalysis data demonstrates that the Sentinel-1 retrievals capture the spatial variability between and within mountain ranges, as well as their inter-annual differences. This is showcased with the contrasting snow depths between 2017 and 2018 in the US Sierra Nevada and European Alps. With Sentinel-1 continuity ensured until 2030 and likely beyond, these findings lay a foundation for quantifying the long-term vulnerability of mountain snow-water resources to climate change.

Original languageEnglish
Article number4629
JournalNature Communications
Volume10
Issue number1
DOIs
Publication statusPublished - 1 Dec 2019

Bibliographical note

Funding Information:
R.R. and M.G. were supported by the NASA Terrestrial Hydrology program. Sentinel-1A/B data are from the ESA and Copernicus Sentinel Satellites project and were processed using Google Earth Engine.

Funding Information:
This work was funded through the BELSPO SNOPOST and C-SNOW projects. Part of the study was performed by H.L. at NASA/GSFC, with computational resources provided by the NASA High-End Computing Program through the Center for Climate Simulation.

Publisher Copyright:
© 2019, The Author(s).

Funding

R.R. and M.G. were supported by the NASA Terrestrial Hydrology program. Sentinel-1A/B data are from the ESA and Copernicus Sentinel Satellites project and were processed using Google Earth Engine. This work was funded through the BELSPO SNOPOST and C-SNOW projects. Part of the study was performed by H.L. at NASA/GSFC, with computational resources provided by the NASA High-End Computing Program through the Center for Climate Simulation.

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