Comparison of the multi-layer HUT snow emission model with observations of wet snowpacks

被引:5
|
作者
Pan, Jinmei [1 ,2 ,3 ,4 ]
Jiang, Lingmei [1 ,2 ,3 ]
Zhang, Lixing [1 ,2 ,3 ]
机构
[1] Beijing Normal Univ, State Key Lab Remote Sensing Sci, Beijing 100875, Peoples R China
[2] Chinese Acad Sci, Inst Remote Sensing Applicat, Beijing 100875, Peoples R China
[3] Beijing Normal Univ, Sch Geog & Remote Sensing Sci, Beijing 100875, Peoples R China
[4] Ohio State Univ, Sch Earth Sci, Columbus, OH 43210 USA
基金
中国国家自然科学基金;
关键词
HUT model; wet snow; passive microwave remote sensing; WATER EQUIVALENT RETRIEVALS; MULTIPLE-SCATTERING MODEL; STRONG FLUCTUATION THEORY; MICROWAVE EMISSION; DRY SNOW; RADIOMETER DATA; BOREAL; DEPTH; SOIL; SIMULATIONS;
D O I
10.1002/hyp.9617
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
Information on snow properties plays an important role in hydrological, meteorological and climatological applications. Passive microwave remote sensing is an effective method to retrieve snowpack parameters; however, the observations can be obscured if there is wet snow in the satellite footprint. To study the emission properties of wet snow and check its response to snow wetness, this paper applies the multi-layer Helsinki University of Technology (HUT) snow emission model coupled with the Advanced Integral Equation Model to simulate the low-wetness snowpack observed at Luancheng in November 2009, and the high wetness snowpack observed at Weissfluhjoch in June 1995. Input parameters are acquired by the in-situ snow pit measurements, while the snow grain size is fitted by comparing model predictions with the observed passive microwave signals at a range of observing angles. Results show that the application of a multi-layer model is capable to consider the distribution pattern of the snow wetness along the snow profile and the refrozen ice crust of the snow surface. The multi-layer HUT model is able to reproduce the wet snow emission properties, with an rms error of 4.4 K (at Luancheng) and 5.7 K (at Weissfluhjoch) at vertical polarization, and an rms error of 7.9 K (at Luancheng) and 11.4 K (at Weissfluhjoch) at horizontal polarization. Copyright (c) 2012 John Wiley & Sons, Ltd.
引用
收藏
页码:1071 / 1083
页数:13
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