WebThe albedo of clean snow is typically higher than 90% by assuming spheri- cal snow grains of ~50 to 200 μm at visible wavelengths (400–750 nm), while the albedo of dirty snow with amounts of black carbon (BC) concentrations (~2000 ng g−1) can de- crease to 70% [1, 2]. WebThe SNICAR model has been used widely to calculate the snow spectral albedo in the fields of atmospheric and cryospheric sciences, 7,37 and also has been coupled with global …
Julian Arnheim - Ph.D. Student - UC Irvine Department of
WebWe implement a set of new parameterizations into the widely used Snow, Ice, and Aerosol Radiative (SNICAR) model to account for effects of snow g... Journal Article OPEN … Web5 Oct 2024 · BioSNICAR predicts the spectral albedo of snow and glacier ice between 200nm to 5000nm given information about the illumination conditions, ice structure and … jfe精密 コーティング
SNICAR-ADv3: a community tool for modeling spectral snow albedo
WebThe new model simulates broadband albedos ranging from 0.03 (bare, bubble-free ice) to 0.88 (fine-grained snow) (Figs. 3 and 4), with non-linear dependencies of LAC-induced albedo change on... http://flanner.engin.umich.edu/wp-content/uploads/sites/544/2024/09/Kuiper11.pdf Web8 Oct 2024 · The estimation by the Snow, Ice, and Aerosol Radiative (SNICAR) model indicated that BC and MD could reduce the albedo by 12.8 and 10.3% in fresh snow, aged … jfe継手 カタログ