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CROSSING SWELL AND ORIGINS: GLOBAL VIEW FROM ASAR WAVE MODE FIREWORKS

机译:跨越波澜和起源:ASAR波模烟花的全球视野

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摘要

Crossing swell, is a complicated sea state characterizedrnby the co-existence of swell systems generating fromrndifferent swell origins. Although many investigationsrnhave focused on the global swell climatology, ourrnunderstanding of global statistical distribution for therncrossing swell is still limited. In this paper, we present arnglobal view of crossing swell using 10-years SyntheticrnAperture Radar (SAR) derived directional swell spectrarnfrom Envisat ASAR in Wave Mode from 2003 to 2011.rnIn contrast to analyze the directly but occasionally SARrncaptured sea state of crossing swell, we employ anrnapproach of propagating observed swell takingrnadvantage of the internal consistency of swells. Resultsrnreveal three dominated crossing swell areas termedrn“crossing swell pools”, in Pacific, Atlantic and IndianrnOceans. The pool in Atlantic Ocean shows a relativernstable behaviour for all seasons, in contrast to the one inrnIndian Ocean with seasonal occurrence and the one inrnPacific Ocean shrinking during boreal summer. Thernsources of the crossing swell are also inferred fromrnASAR wave mode data, and its global distributionrnanalysis results indicate good agreement with thernseasonal variation of crossing swell pools.
机译:穿越海浪是一种复杂的海洋状态,其特征是由不同的海浪起源产生的海浪系统并存。尽管许多研究都集中在全球涌浪气候学上,但我们对穿越浪涌的全球统计分布的理解仍然有限。本文以2003年至2011年的10年合成波孔径雷达(SAR)的Envisat ASAR定向波谱为研究对象,以波模式展示了交叉波的全貌。采用传播观察到的膨胀的方法,利用膨胀内部一致性的优势。结果在太平洋,大西洋和印度洋中,三个主要的交叉隆起区被称为“交叉隆起池”。大西洋中的水池在所有季节中都表现出相对稳定的行为,与之相反的是,一个印度洋具有季节性发生,而一个印度洋则在夏季北方萎缩。还可以从ASAR波模式数据中推断出交叉隆起的来源,其整体分布分析结果表明与交叉隆起的季节变化有很好的一致性。

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  • 来源
  • 会议地点 Wuhan(CN)
  • 作者单位

    National Ocean Technology Center, 219 JieYuanXi Rd,Tianjin China, Email: wanghe_sio@126.com;

    Ifremer, Plouzane, France, Email: alexis.mouche@ifremer.fr;

    Collecte Localisation Satellites, Plouzane, France, Email: rhusson@cls.fr;

    Ifremer, Plouzane, France bertrand.chapron@ifremer.fr;

    State Key Laboratory of Satellite Ocean Environment Dynamics, Second Institute of Oceanography, State OceanicAdministration, Hangzhou, China, Email: jsyang@sio.org.cn;

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