首页> 外文会议>第21届国际摄影测量与遥感大会(ISPRS 2008)论文集 >CONTRIBUTION OF THE YANGTZE RIVER TO ECOSYSTEM OF THE EAST CHINA SEA
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CONTRIBUTION OF THE YANGTZE RIVER TO ECOSYSTEM OF THE EAST CHINA SEA

机译:长江对东海生态系统的贡献

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The Yangtze River of the China main land has recorded the decrease of sediment load in these 10 years because of construction of dams in the upstream region. The Three Gorgeous Dam, partly started its operation since July of 2003, has a significant contribution to reduce the sediment load with sedimentation. According to the Yangtze River hydrological report, the amount of discharge and the sediment concentration exhibit a clear migration in season and temporal changes. The seasonal and annual variations of discharge and sediment concentration are expected to have a strong contribution to the ecosystem in the East China Sea. In this study, a primary productivity in the East China Sea, especially over the offshore region of the Yangtze River mouth, is estimated with satellite monitoring of chlorophyll-a concentration, sea surface temperature, photo-synthetically available radiation, which are observed by MODIS on the polar orbiting satellite AQUA. The depth resolved primary productivity model was implemented to estimate the primary productivity where sufficient amount of nutrients are supplied and the variation of environments by the river compounds. In-situ measurements are also conducted at the entrance of the Kuroshio into the East China Sea, at one exit of the Kuroshio into the Pacific and at another exit of the Kuroshio into the Japan Sea to monitor effects of the Yangtze River. The in-situ measurements were conducted to evaluate the extensions of diluted water into the Kuroshio in the spring, when the discharge exhibits lower value, and in the summer, when the discharge exhibits the maximum value through the year. This paper discusses the contribution of the Yangtze River to the ecosystem of the East China Sea through the primary productivity and the effects of the diluted water into the Kuroshio.
机译:由于上游地区的水坝建设,这十年来中国主要土地的长江录得泥沙负荷减少。三峡大坝从2003年7月开始部分运行,为减少沉积物中的泥沙负荷做出了重大贡献。根据长江水文报告,流量和泥沙浓度在季节和时间变化中表现出明显的迁移。预计排放量和沉积物浓度的季节和年度变化将对东中国海的生态系统做出重要贡献。在这项研究中,通过卫星监测叶绿素-a浓度,海面温度,光合有效辐射(通过MODIS观测),估算了东海特别是长江口近海地区的初级生产力。在极地轨道卫星AQUA上。实施了深度分解的初级生产力模型,以估算提供足够养分和河流化合物造成的环境变化的初级生产力。还对黑潮进入东中国海的入口,黑潮进入太平洋的一个出口以及黑潮进入日本海的另一个出口进行了现场测量,以监测长江的影响。在春季,当排放量显示较低的值时,以及在夏天,当排放量显示全年的最大值时,进行了现场测量,以评估稀释水向黑潮的扩散。本文讨论了长江通过初级生产力对东海生态系统的贡献以及稀释水对黑潮的影响。

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