首页> 外文会议>International symposium on remote sensing;ISRS >THE SPATIAL-TEMPORAL VARIABILITY OF CHANGJIANG DILUTED WATER USING SATELLITE AND MODEL DATA IN EAST CHINA SEA
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THE SPATIAL-TEMPORAL VARIABILITY OF CHANGJIANG DILUTED WATER USING SATELLITE AND MODEL DATA IN EAST CHINA SEA

机译:利用卫星和模型数据对长江淡水的时空变化特征

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The East China Sea (ECS) is passage connect Pacific with sea area near Korean peninsula, flow in fresh water and terrigenous sediments through Changjiang river of China. Especially, Changjiang Diluted Water (CDW) is formed by fresh water of Changjiang river and sea water of the ECS and influenced into the East/Japan Sea include Jeju Island during summer season. The purpose of this study is to trace CDW and analysis spatial displacement of CDW's distribution during summer season from 2009 to 2016. In this study, we used surface salinity and velocity data of Hybrid Coordinate Ocean Model (HYCOM). The ocean color data, MODIS-Aqua, used for understand spatial change of CDW. This study performed particle tracking to find trajectory of low-salinity water using daily surface velocity, which started near the Changjiang mouth with low salinity boundary under 31 psu. To calculating the spatial and temporal variations of CDW, we simulated the particle tracking with daily surface salinity and compared with ocean color data. The displacement of CDW is affected by amount of Changjiang River Discharge (CRD), wind direction on the ECS. The particle tracking and ocean color data greatly increases of understand the spatial and temporal variations for determining CDW pathway and its influence.
机译:东中国海(ECS)是连接太平洋与朝鲜半岛附近海域的通道,淡水和陆源沉积物流经中国长江。尤其是长江淡水(CDW)是由长江淡水和ECS的海水形成的,并在夏季进入济州岛的东/日本海。本研究的目的是追踪CDW并分析2009年至2016年夏季CDW分布的空间位移。在本研究中,我们使用了混合坐标海洋模型(HYCOM)的地表盐度和速度数据。海洋颜色数据MODIS-Aqua用于了解CDW的空间变化。这项研究利用每日表面速度进行了颗粒追踪,以找到低盐度水的轨迹,该表面速度始于长江口附近,盐分边界低于31 psu的低盐度。为了计算CDW的时空变化,我们模拟了具有每日表面盐度的粒子跟踪,并与海洋颜色数据进行了比较。 CDW的位移受长江排量(CRD)和ECS上的风向的影响。粒子追踪和海洋颜色数据大大增加了对确定CDW途径及其影响的时空变化的理解。

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