["Chernenkov, A. Yu","Kostrykin, S., V"]2021-03-01期刊论文
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Using a balance model of the snow layer, we estimate the concentration of black carbon (BC) in the snow; then, with the help of radiative transfer model SNICAR, we calculate the snow albedo and radiative forcing (RF) from snow darkening with BC. Data from an ensemble simulation with INMCM5, the 5th version of the climate model of Marchuk Institute of Numerical Mathematics, Russian Academy of Sciences for the period 1998-2002 are used as input, which include snow both on land and on sea ice. The regionally averaged results are compared with other model data and field measurements.
