A temporal sliding procedure for ocean wave variational data assimilation and its application
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A temporal sliding procedure for ocean wave variational data assimilation and its application
A temporal sliding procedure for ocean wave variational data assimilation and its application
海洋湖沼学报(英文)2006年24卷第1期 页码:35-41
Affiliations:
1. First Institute of Oceanography SOA
2. Key Laboratory of Marine Science and Numerical Modeling SOA
Author bio:
Funds:
Supported by the High-Tech Research and Development Program of China (863 Program. No. 2001AA633070;2003AA604040), and National Natural Science Foundation of China (No. 40206003).
A temporal sliding procedure for ocean wave variational data assimilation and its application[J]. 海洋湖沼学报(英文), 2006,24(1):35-41.
Yongzeng, Y., Wei, Z. & Yong, T. A temporal sliding procedure for ocean wave variational data assimilation and its application., Chin. J. Ocean. Limnol. 24, 35–41 (2006). https://doi.org/10.1007/BF02842772
A temporal sliding procedure for ocean wave variational data assimilation and its application[J]. 海洋湖沼学报(英文), 2006,24(1):35-41. DOI: 10.1007/BF02842772.
Yongzeng, Y., Wei, Z. & Yong, T. A temporal sliding procedure for ocean wave variational data assimilation and its application., Chin. J. Ocean. Limnol. 24, 35–41 (2006). https://doi.org/10.1007/BF02842772DOI:
A temporal sliding procedure for ocean wave variational data assimilation and its application
摘要
Abstract
For sequential performance of wave variational data assimilation
we proposed a temporal sliding method in which the temporal overlap is considered. The advantage of this method is that the initial wave spectrum of the optimization process is modified by the observations in latter and former times. This temporal sliding procedure is important for marginal region
such as the China seas
where the duration of assimilation effectiveness is 2–3 days. Experiments were performed in the whole course of Cyclone 9403 (Russ). Around the cyclone center
the maximum value of wave elements did not change much by assimilation
because the extreme value was determined by wind energy input that was not yet optimized. In the area outside the cyclone center
this modification is evident especially for wind wave growth.
关键词
Keywords
references
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