Inter-Calibration of Passive Microwave Satellite Brightness Temperatures Observed by F13 SSM/I and F17 SSMIS for the Retrieval of Snow Depth on Arctic First-Year Sea Ice

被引:7
|
作者
Liu, Qingquan [1 ]
Ji, Qing [1 ,2 ]
Pang, Xiaoping [1 ,2 ]
Gao, Xin [3 ]
Zhao, Xi [1 ,2 ]
Lei, Ruibo [4 ]
机构
[1] Wuhan Univ, Chinese Antarctic Ctr Surveying & Mapping, Wuhan 430079, Hubei, Peoples R China
[2] Natl Adm Surveying Mapping & Geoinformat, Key Lab Polar Surveying & Mapping, Wuhan 430079, Hubei, Peoples R China
[3] Wuhan Univ, Sch Resource & Environm Sci, Wuhan 430079, Hubei, Peoples R China
[4] State Ocean Adm, Polar Res Inst China, Key Lab Polar Sci, Shanghai 200136, Peoples R China
基金
中国国家自然科学基金;
关键词
snow depth; SSM; I; SSMIS; Operation IceBridge; Arctic; THICKNESS; PRODUCTS;
D O I
10.3390/rs10010036
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Passive microwave satellite brightness temperatures (TB) that were observed by the F13 Special Sensor Microwave/Imager (SSM/I) and the subsequent F17 Special Sensor Microwave Imager/Sounder (SSMIS) were inter-calibrated using empirical relationship models during their overlap period. Snow depth (SD) on the Arctic first-year sea ice was further retrieved. The SDs derived from F17 TB and F13C TB which were calibrated F17 TB using F13 TB as the baseline were then compared and evaluated against in situ SD measurements based on the Operational IceBridge (OIB) airborne observations from 2009 to 2013. Results show that Cavalieri inter-calibration models (CA models) perform smaller root mean square error (RMSE) than Dai inter-calibration models (DA models), and the standard deviation of OIB SDs in the 25 km pixels is around 6 cm on first-year sea ice. Moreover, the SDs derived from the calibrated F17 TB using F13 TB as the baseline were in better agreement than the F17 SDs as compared with OIB SDs, with the biases of -2 cm (RMSE of 5 cm) and -9 cm (RMSE of 10 cm), respectively. We conclude that TB observations from F17 SSMIS calibrated to F13 SSM/I as the baseline should be recommended when performing the sensors' biases correction for SD purpose based on the existing algorithm. These findings could serve as a reference for generating more consistent and reliable TB, which could help to improve the retrieval and analysis of long-term snow depth on the Arctic first-year sea ice.
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页数:12
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