Quantifying Relative Contributions of Light-Absorbing Particles From Domestic and Foreign Sources on Snow Melt at Sapporo, Japan During the 2011-2012 Winter

被引:9
|
作者
Niwano, M. [1 ,2 ]
Kajino, M. [1 ,3 ]
Kajikawa, T. [4 ]
Aoki, T. [2 ]
Kodama, Y. [5 ]
Tanikawa, T. [1 ]
Matoba, S. [6 ]
机构
[1] Japan Meteorol Agcy, Meteorol Res Inst, Tsukuba, Ibaraki, Japan
[2] Natl Inst Polar Res, Tachikawa, Tokyo, Japan
[3] Univ Tsukuba, Fac Life & Environm Sci, Tsukuba, Ibaraki, Japan
[4] Univ Tsukuba, Grad Sch Sci & Technol, Tsukuba, Ibaraki, Japan
[5] Hokkaido Univ, Arctic Res Ctr, Sapporo, Hokkaido, Japan
[6] Hokkaido Univ, Inst Low Temp Sci, Sapporo, Hokkaido, Japan
基金
日本学术振兴会;
关键词
light-absorbing particles; seasonal snow; physical snowpack model; regional meteorology-chemistry model; radiative forcing; snow cover duration; NONSPHERICAL ICE PARTICLE; BLACK CARBON; UNCERTAINTY ASSESSMENT; INDEPENDENT SPHERES; ELEMENTAL CARBON; SPECTRAL ALBEDO; GRAIN SHAPE; IN-SITU; MODEL; AEROSOL;
D O I
10.1029/2021GL093940
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Depositions of light-absorbing particles (LAPs), such as black carbon (BC) and dust, on the snow surface modulate the snow albedo; therefore, they are considered key factors of snow-atmosphere interaction in the present-day climate system. However, their detailed roles have not yet been fully elucidated, mainly due to the lack of in-situ measurements. Here, we develop a new model chain NHM-Chem-SMAP, which is composed of a detailed regional meteorology-chemistry model and a multilayered physical snowpack model, and evaluate it using LAPs concentrations data measured at Sapporo, Japan during the 2011-2012 winter. NHM-Chem-SMAP successfully reproduces the in-situ measured seasonal variations in the mass concentrations of BC and dust in the surface snowpack. Furthermore, we find that LAPs from domestic and foreign sources played a role in shortening the snow cover duration by 5 and 10 days, respectively, compared to the completely pure snow condition.
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页数:10
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