GSTDTAP  > 气候变化
DOI10.1029/2018GL081029
Ocean Surface Wave-Current Signatures From Satellite Altimeter Measurements
Quilfen, Y.; Chapron, B.
2019-01-16
发表期刊GEOPHYSICAL RESEARCH LETTERS
ISSN0094-8276
EISSN1944-8007
出版年2019
卷号46期号:1页码:253-261
文章类型Article
语种英语
国家France
英文摘要

Ocean currents can strongly impact the propagation of swell systems. Satellite altimetry routinely provides measurements of ocean surface significant wave heights (Hs). A self-consistent space-scale decomposition is applied to Hs measurements obtained from different altimeters. This method helps reveal overlooked statistical properties at scales less than 100km, where mesoscale and submesoscale upper ocean circulation drives a significant part of the variability in the coupled ocean-atmosphere system. In particular, systematic signatures related to wave-current interactions are clear at global and regional scales. In the Agulhas current system, the proposed space-scale decomposition further reveals organized and persistent patterns. To leading order, the redistribution of swell energy follows the cumulative impact of the large-scale current vorticity field on wave train kinematics. This relationship causes significant swell ray deflection and localized trapping phenomena, which are adequately captured by altimeter measurements.


Plain Language Summary Long and energetic surface waves radiating from distant storms may eventually cover a full ocean basin with a lifetime that can extend over a few weeks. Chances are that these swell fields will propagate over regions characterized by strong ambiant upper ocean currents. Resulting interactions can then trigger sea state variability, including the formation of severe crossing sea conditions. To better document these anticipated effects at global and regional scales, a new methodology is applied to best exploit multisatellite altimeter measurements. As obtained, the resulting augmented data sets provide an unprecedented evidence of the co-variability of surface waves and currents over all ocean basins. More regionally, the analysis shows that persistent and localized sea state anomalies in the Agulhas current region are well explained by swell refraction and focusing effects in the variable current stream. The proposed methodology opens new perspectives for studies and applications combining numerical modeling and satellite observations.


英文关键词altimeter observations wave-current interactions denoising method
领域气候变化
收录类别SCI-E
WOS记录号WOS:000456938600028
WOS关键词EMPIRICAL MODE DECOMPOSITION ; REFRACTION ; CIRCULATION ; AGULHAS ; SERIES ; SWELL
WOS类目Geosciences, Multidisciplinary
WOS研究方向Geology
引用统计
文献类型期刊论文
条目标识符http://119.78.100.173/C666/handle/2XK7JSWQ/26829
专题气候变化
作者单位Univ Brest, IFREMER, Lab Oceanog Phys & Spatiale, CNRS,IRD,IUEM, Brest, France
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GB/T 7714
Quilfen, Y.,Chapron, B.. Ocean Surface Wave-Current Signatures From Satellite Altimeter Measurements[J]. GEOPHYSICAL RESEARCH LETTERS,2019,46(1):253-261.
APA Quilfen, Y.,&Chapron, B..(2019).Ocean Surface Wave-Current Signatures From Satellite Altimeter Measurements.GEOPHYSICAL RESEARCH LETTERS,46(1),253-261.
MLA Quilfen, Y.,et al."Ocean Surface Wave-Current Signatures From Satellite Altimeter Measurements".GEOPHYSICAL RESEARCH LETTERS 46.1(2019):253-261.
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