Analysis of Arctic seas surface wind field and ocean wave remote sensing observation capability

Yang Jungang; Zhang Jie; Wang Guizhong

doi:10.3969/j.issn.0253-4193.2018.11.011

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Yang Jungang, Zhang Jie, Wang Guizhong. Analysis of Arctic seas surface wind field and ocean wave remote sensing observation capability[J]. Haiyang Xuebao, 2018, 40(11): 105-115. doi: 10.3969/j.issn.0253-4193.2018.11.011

Citation:

Yang Jungang, Zhang Jie, Wang Guizhong. Analysis of Arctic seas surface wind field and ocean wave remote sensing observation capability[J]. Haiyang Xuebao, 2018, 40(11): 105-115. doi: 10.3969/j.issn.0253-4193.2018.11.011

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Analysis of Arctic seas surface wind field and ocean wave remote sensing observation capability

doi: 10.3969/j.issn.0253-4193.2018.11.011

1.
The First Institute of Oceanography, State Oceanic Administration, Qingdao 266061, China
2.
College of Information and Engineering, Ocean University of China, Qingdao 266003, China

Received Date: 2018-01-20
Rev Recd Date: 2018-02-27

Abstract

Abstract

Satellite remote sensing is an important method to study the distribution and variation of sea surface winds and ocean waves in the Arctic seas. Based on remote sensing data of the orbiting multi-source satellites, the observation capability of the sea surface wind and the ocean wave in the Arctic Ocean is analyzed from three aspects:spatial coverage of remote sensing observations, time coverage and remote sensing data merging. It is concluded as follows. The ASCAT and HY-2A scatterometers can be used for sea surface wind remote sensing observation in the Arctic seas and the multi-satellite joint observation can obtain the sea surface wind remote sensing data with the spatial and temporal resolution of better than 12 hours and 0.1° in the Arctic Ocean. Based on the HY-2A, CryoSat-2, SARAL and Sentinel-3 altimeters, the remote sensing observations of the Arctic seas waves can be realized. The multi-satellite joint observations can obtain the ocean wave remote sensing data of the spatial and temporal resolution of 1 day and 0.25° in the Arctic seas. Based on sea surface wind and ocean wave fusion data in 2016, it is concluded that sea surface wind and ocean wave in the Arctic seas are high from January to March and then decrease to the minimum in July, then gradually increase. The results show that sea surface wind and ocean wave in the Arctic seas can be monitored by multi-source scatterometers and altimeters with high spatial and temporal resolution.
- Arctic,
- sea surface wind,
- ocean wave,
- remote sensing observation

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References(14)

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