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- W4200599100 abstract "<strong class=journal-contentHeaderColor>Abstract.</strong> This study investigates the sensitivity of modeled surface melt and subsurface heating on the Antarctic ice sheet to a new spectral snow albedo and radiative transfer scheme in the Regional Atmospheric Climate Model (RACMO), version 2.3p3 (Rp3). We tune Rp3 to observations by performing several sensitivity experiments and assess the impact on temperature and melt by incrementally changing one parameter at a time. When fully tuned, Rp3 compares well with in situ and remote sensing observations of surface mass and energy balance, melt, near-surface and (sub)surface temperature, albedo and snow grain specific surface area. Near-surface snow temperature is especially sensitive to the prescribed fresh snow specific surface area and fresh dry snow metamorphism. These processes, together with the refreezing water grain size and subsurface heating, are important for melt around the margins of the Antarctic ice sheet. Moreover, small changes in the albedo and the aforementioned processes can lead to an order of magnitude overestimation of melt, locally leading to runoff and a reduced surface mass balance." @default.
- W4200599100 created "2021-12-31" @default.
- W4200599100 creator A5019954380 @default.
- W4200599100 date "2021-12-24" @default.
- W4200599100 modified "2023-09-29" @default.
- W4200599100 title "Reply on RC1, RC2 and RC3" @default.
- W4200599100 doi "https://doi.org/10.5194/tc-2021-298-ac1" @default.
- W4200599100 hasPublicationYear "2021" @default.
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