Retrieving snow depth distribution by downscaling ERA5 Reanalysis with ICESat-2 laser altimetry

• URL: http://arxiv.org/abs/2410.17934v1
• Date: Wed, 23 Oct 2024 14:59:06 GMT
• Title: Retrieving snow depth distribution by downscaling ERA5 Reanalysis with ICESat-2 laser altimetry
• Authors: Zhihao Liu, Simon Filhol, Désirée Treichler,
• Abstract summary: This study uses snow depth measurements from the ICESat-2 satellite laser altimeter to produce snow depth maps at microscale (10 m) A regression model is fitted to establish a relationship between the retrieved snow depth and the corresponding ERA5 Land snow depth. The method can provide timeseries of monthly snow depth maps for the entire ERA5 time range (since 1950)
• Score: 2.5124917269950324
• License:
• Abstract: Estimating the variability of seasonal snow cover, in particular snow depth in remote areas, poses significant challenges due to limited spatial and temporal data availability. This study uses snow depth measurements from the ICESat-2 satellite laser altimeter, which are sparse in both space and time, and incorporates them with climate reanalysis data into a downscaling-calibration scheme to produce monthly gridded snow depth maps at microscale (10 m). Snow surface elevation measurements from ICESat-2 along profiles are compared to a digital elevation model to determine snow depth at each point. To efficiently turn sparse measurements into snow depth maps, a regression model is fitted to establish a relationship between the retrieved snow depth and the corresponding ERA5 Land snow depth. This relationship, referred to as subgrid variability, is then applied to downscale the monthly ERA5 Land snow depth data. The method can provide timeseries of monthly snow depth maps for the entire ERA5 time range (since 1950). The validation of downscaled snow depth data was performed at an intermediate scale (100 m x 500 m) using datasets from airborne laser scanning (ALS) in the Hardangervidda region of southern Norway. Results show that snow depth prediction achieved R2 values ranging from 0.74 to 0.88 (post-calibration). The method relies on globally available data and is applicable to other snow regions above the treeline. Though requiring area-specific calibration, our approach has the potential to provide snow depth maps in areas where no such data exist and can be used to extrapolate existing snow surveys in time and over larger areas. With this, it can offer valuable input data for hydrological, ecological or permafrost modeling tasks.

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