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利用海洋2B卫星数据反演南极海冰表面积雪厚度

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海冰及其表面积雪厚度是大气和海洋间的能量循环和物质平衡的重要因子,是对气候环境变化的敏感指示器.本文尝试利用国产海洋2B卫星(HY-2B)数据开展南极海冰表面积雪厚度遥感反演的研究.结果表明:基于2018年 11月至2019年1月我国第35次南极科学考察"雪龙船"走航观测的积雪厚度数据,Comiso03积雪厚度遥感反演模型相对于Markus98模型和Shen22模型反演的南极海冰表面积雪厚度精度最好,时空平均偏差为-1.88 cm.基于搭载在HY-2B上的扫描微波辐射计(scanning microwave radiome-ter,SMR)所反演的南极海冰表面积雪厚度与基于搭载在地球水环境变动监测卫星(Global Change Observation Mission 1st-Water,GCOM-W1)上的先进微波扫描辐射计(the ad-vanced microwave scanning radiometer-2,AMSR-2)发布的积雪厚度产品(Comiso03模型)具有较好的一致性,两者间的差异主要发生在消融期,在空间分布上的差异主要集中在南极印度洋扇区和西太平洋扇区.利用HY-2B SMR数据反演南极海冰表面积雪厚度的研究可为应用国产海洋卫星系列数据开展长时序南极海冰及其表面积雪的变化研究提供重要的数据和技术支撑.
Retrieval of Snow Depth on Antarctic Sea Ice Using HY-2B Satellite Data
Sea ice and its surface snow depth are important factors of energy cycle and mass balance between atmosphere and ocean,and sensitive indicators of climate and environmen-tal change.This study attempts to apply Chinese HY-2B Sat-ellite Data to retrieve snow depth on Antarctic Sea ice.Re-sults show that the remote sensing retrieval model of Comio-so03 has the best accuracy with a spatial-temporal averaged deviation of-1.88 cm compared with that of Markus98 mod-el and Shen22 model against the snow measurements during the 35th Antarctic Scientific Expedition of China from the No-vember 2018 to January 2019.The HY-2B SMR snow depth on Antarctic sea ice is in good agreement with the GCOM-W1 AMSR-2 snow depth product(Comisto03 model).The difference between them mainly occurs in the sea ice ablation period and concentrate in the Antarctic Indian Ocean sector and the Western Pacific Ocean sector.Research on the re-mote sensing retrieval of snow depth on Antarctic Sea ice based on HY-2B SMR data could provide important data and technical support for the application of Chinese marine satel-lite series data to monitor long-term Antarctic Sea ice and snow changes.

snow depthsea iceHY-2Bpassive micro-wave remote sensingAntarctic

肖泽辉、季青、庞小平、闫忠男

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武汉大学中国南极测绘研究中心,湖北,武汉,430079

自然资源部极地测绘重点实验室,湖北,武汉,430079

积雪厚度 海冰 HY-2B 被动微波遥感 南极

2024

测绘地理信息
武汉大学

测绘地理信息

CSTPCD
影响因子:0.563
ISSN:1007-3817
年,卷(期):2024.49(6)