Reanalysis Surface Mass Balance of the Greenland Ice Sheet Along K‐Transect (2000–2014)

نویسندگان

چکیده

Abstract Accurate estimates of surface mass balance over the Greenland ice sheet (GrIS) would contribute to understanding cause recent changes and help better estimate future contribution GrIS sea‐level rise. Given limitations in‐situ measurements, modeling, remote sensing, it is critical explore opportunity merge available data characterize spatial temporal variation (SMB). This work utilizes a particle batch smoother assimilation technique that yields SMB benefit from snow model Crocus 16‐day albedo product derived satellite sensing data. Comparison results against measurements shows reduces root mean square error posterior by 51% bias 95%.

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ژورنال

عنوان ژورنال: Geophysical Research Letters

سال: 2021

ISSN: ['1944-8007', '0094-8276']

DOI: https://doi.org/10.1029/2021gl094602