首页> 外文会议>International symposium on multispectral image processing and pattern recognition;MIPPR 2011 >The distribution, sources and propagation of internal waves in South China Sea based on satellite remote sensing
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The distribution, sources and propagation of internal waves in South China Sea based on satellite remote sensing

机译:基于卫星遥感的南海内波分布,来源和传播

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In this paper, more than 1000 SAR (ENVISAT, ERS-2) and optical (MODIS, HJ-1A/1B) images are used to analyze the distribution, sources and propagation of internal waves in South China Sea. The distribution of internal waves shows that, internal waves mainly occur in three regions of South China Sea: 1) Northern South China Sea, 2) Western South China Sea, 3) Southern South China Sea. Internal waves are observed all year in the South China Sea, most during summer, least in winter. The sources and propagation of internal waves are obtained from the distribution of internal waves. 1) in Northern South China Sea, most internal waves origin in Luzon Strait and propagate westward across Dongsha Island, then some internal waves turn into northwestward, others continue to propagate westward.2) in Western South China Sea, internal waves generate at the shelf, and propagate to the shore or off the shore.3) in Southern South China Sea, internal waves generate at the shelf. Some internal waves propagate to the Kalimantan shore, some propagate southwestward.
机译:本文利用1000多个SAR(ENVISAT,ERS-2)和光学(MODIS,HJ-1A / 1B)图像来分析南海内波的分布,来源和传播。内部波的分布表明,内部波主要发生在南海的三个区域:1)南海北部; 2)南海西部; 3)南海南部。在南海,全年都观测到内波,大部分发生在夏季,最小的是冬季。内部波的来源和传播是从内部波的分布中获得的。 1)在南海北部,大部分内波起源于吕宋海峡,并向西传播穿过东沙岛,然后一些内波向西北传播,另一些内波继续向西传播。2)在南海西部,内波在架子上产生3)在南海南部,陆架内部产生了海浪。一些内部波传播到加里曼丹海岸,另一些向西南传播。

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