The sensitivity of landfast sea ice to atmospheric forcing in single-column model simulations: a case study at Zhongshan Station, Antarctica
Fengguan Gu,Qinghua Yang,Frank Kauker,Changwei Liu,Guanghua Hao,Chao-Yuan Yang,Jiping Liu,Petra Heil,Xuewei Li,and Bo Han
Fengguan Gu
School of Atmospheric Sciences, Sun Yat-sen University, and Southern
Marine Science and Engineering Guangdong Laboratory (Zhuhai), Zhuhai 519082,
China
School of Atmospheric Sciences, Sun Yat-sen University, and Southern
Marine Science and Engineering Guangdong Laboratory (Zhuhai), Zhuhai 519082,
China
School of Atmospheric Sciences, Sun Yat-sen University, and Southern
Marine Science and Engineering Guangdong Laboratory (Zhuhai), Zhuhai 519082,
China
Guanghua Hao
Key Laboratory of Marine Hazards Forecasting, National Marine
Environmental Forecasting Center, Ministry of
Natural Resources, Beijing 100081, China
School of Atmospheric Sciences, Sun Yat-sen University, and Southern
Marine Science and Engineering Guangdong Laboratory (Zhuhai), Zhuhai 519082,
China
Jiping Liu
Department of Atmospheric and Environmental Sciences, State University of
New York at Albany, Albany, NY, USA
School of Atmospheric Sciences, Sun Yat-sen University, and Southern
Marine Science and Engineering Guangdong Laboratory (Zhuhai), Zhuhai 519082,
China
School of Atmospheric Sciences, Sun Yat-sen University, and Southern
Marine Science and Engineering Guangdong Laboratory (Zhuhai), Zhuhai 519082,
China
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The sea ice thickness was simulated by a single-column model and compared with in situ observations obtained off Zhongshan Station in the Antarctic. It is shown that the unrealistic precipitation in the atmospheric forcing data leads to the largest bias in sea ice thickness and snow depth modeling. In addition, the increasing snow depth gradually inhibits the growth of sea ice associated with thermal blanketing by the snow.
The sea ice thickness was simulated by a single-column model and compared with in situ...
