| FAN Xiaopeng,ZHOU Feng,CHEN Xueen,HUANG Daji,POHLMANN Thomas.The influence of the Three-Gorges Dam on hydrographic and hydrodynamic conditions of the East China Sea[J].Acta Oceanologica Sinica,2011,(5):45-55 |
| The influence of the Three-Gorges Dam on hydrographic and hydrodynamic conditions of the East China Sea |
| The influence of the Three-Gorges Dam on hydrographic and hydrodynamic conditions of the East China Sea |
| 投稿时间：2011-01-23 修订日期：2011-06-14 |
| DOI：10.1007/s13131-011-0146-z |
| 中文关键词: Three-Gorges-Dam surface salinity anomalies stratification East China Sea |
| 英文关键词:Three-Gorges-Dam surface salinity anomalies stratification East China Sea |
| 基金项目:The Public Science and Technology Research Funds Projects of Ocean under contract Nos 200905001 and 201005019; the Germany-China Cooperation in Marine Science and Technology under contract No. CHN 04/009; the State Basic Research Program of China under contract No.2011CB409803; the State Key Technology Research and Development Program of China under contract No.2008BAC42B03; the Hi-tech Research Development Program of China under Grant No.2007AA09Z117; the National Natural Science Foundation of China under contract No.40706018; the Scientific Research Fund of the Second Institute of Oceanography, the State Oceanic Administration of China under contract Nos JT1105 and JT0903. |
| 作者 | 单位 | E-mail | | FAN Xiaopeng | State Key Laboratory of Satellite Ocean Environment Dynamics, Second Institute of Oceanography, State Oceanic Administration, Hangzhou 310012, China | | | ZHOU Feng | State Key Laboratory of Satellite Ocean Environment Dynamics, Second Institute of Oceanography, State Oceanic Administration, Hangzhou 310012, China
Department of Ocean Science and Engineering, Zhejiang University, Hangzhou 310058, China | | | CHEN Xueen | Institute of Physical Oceanography, Ocean University of China, Qingdao 266002, China | | | HUANG Daji | State Key Laboratory of Satellite Ocean Environment Dynamics, Second Institute of Oceanography, State Oceanic Administration, Hangzhou 310012, China
Department of Ocean Science and Engineering, Zhejiang University, Hangzhou 310058, China | | | POHLMANN Thomas | Institute of Oceanography, University of Hamburg, Hamburg 20146, Germany | thomas.pohlmann@zmaw.de |
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| 中文摘要: |
| A fine resolution model has been applied to get more insight into the effects of a modified runoff due to the Three-Gorges-Dam (TGD) on the East China Sea (ECS). The region of interest was confined to the offshore area in the vicinity of the Changjiang River. To the east, it extended up to the area southwest of Cheju Island. The model was used to evaluate the effect of a modified runoff on the water properties of the adjacent regions like the Changjiang diluted water (CDW) and the Zhoushan Fishing Ground. The sensitivity of the ECS to a modified Changjiang runoff was explored firstly by sensitivity studies and secondly by experiments based on historical runoff records and water management plans of the TGD. These experiments led to the general conclusion that the most affected area by runoff is located close to the Changjiang River mouth. The area of influence has an extension of about 150 km×150 km. In the realistic experiment, the related anomalies reached their maximum value in early summer (May). In normal years the related salinity anomalies can get to as large as 2. |
| 英文摘要: |
| A fine resolution model has been applied to get more insight into the effects of a modified runoff due to the Three-Gorges-Dam (TGD) on the East China Sea (ECS). The region of interest was confined to the offshore area in the vicinity of the Changjiang River. To the east, it extended up to the area southwest of Cheju Island. The model was used to evaluate the effect of a modified runoff on the water properties of the adjacent regions like the Changjiang diluted water (CDW) and the Zhoushan Fishing Ground. The sensitivity of the ECS to a modified Changjiang runoff was explored firstly by sensitivity studies and secondly by experiments based on historical runoff records and water management plans of the TGD. These experiments led to the general conclusion that the most affected area by runoff is located close to the Changjiang River mouth. The area of influence has an extension of about 150 km×150 km. In the realistic experiment, the related anomalies reached their maximum value in early summer (May). In normal years the related salinity anomalies can get to as large as 2. |
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