TY - JOUR
T1 - Snow Depth Variability in the Northern Hemisphere Mountains Observed from Space
AU - Lievens, Hans
AU - Demuzere, Matthias
AU - Marshall, Hans Peter
AU - Reichle, Rolf H.
AU - Brucker, Ludovic
AU - Brangers, Isis
AU - de Rosnay, Patricia
AU - Dumont, Marie
AU - Girotto, Manuela
AU - Immerzeel, Walter W.
AU - Jonas, Tobias
AU - Kim, Edward J.
AU - Koch, Inka
AU - Marty, Christoph
AU - Saloranta, Tuomo
AU - Schöber, Johannes
AU - De Lannoy, Gabrielle J.M.
N1 - Publisher Copyright:
© 2019, The Author(s).
PY - 2019/10/11
Y1 - 2019/10/11
N2 - 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.
AB - 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.
KW - cryospheric science
KW - hydrology
UR - https://www.scopus.com/pages/publications/85073165596
U2 - 10.1038/s41467-019-12566-y
DO - 10.1038/s41467-019-12566-y
M3 - Article
C2 - 31604957
VL - 10
JO - Nature Communications
JF - Nature Communications
IS - 1
M1 - 4629
ER -