RESOURCES AND ENVIRONMENT IN THE YANGTZE BASIN >> 2017, Vol. 26 >> Issue (04): 572-584.doi: 10.11870/cjlyzyyhj201704010

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TEMPORAL AND SPATIAL SIMULATION OF WATER LEVEL AND VELOCITY DURING LOW WATER LEVEL STATISTICAL YEAR IN LAKE POYANG

QI Ling-yan1,2, HUANG Jia-cong1, GAO Jun-feng1, GUO Yu-yin3   

  1. 1. Key Laboratory of Watershed Geographic Sciences, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing 210008, China;
    2. University of Chinese Academy of Sciences, Beijing 100049, China;
    3. Jiangxi Province Poyang Lake Hydrology Bureau, Jiujiang 332800, China
  • Received:2016-09-14 Revised:2016-12-26 Online:2017-04-20
  • Supported by:
    The National Basic Research Program of China (2012CB417006);The Major Water Resources Science and Technology Program of the Jiangxi Water Resources Department (KT201406)

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Abstract: Lake Poyang, as a large lake naturally connected to the Yangtze River, owns different hydrological characteristics. Water level and velocity are the key environmental driving factors to maintain ecological function of the lake aquatic ecosystem. In this paper, EFDC (Environmental Fluid Dynamics Code) was constructed to simulate the water level and water velocity changes in Lake Poyang during the low water level statistical year (from June 30, 2011 to July 1, 2010). And the hydrological data including water level and discharge from five inflow rivers and Hukou station, meteorological data and DEM were as input files to run the model. The paper drew the following conclusions, (1) The simulation results of four hydrological stations showed great fit (r2>0.85). (2)During the high water level period, there was no obvious spatial difference among water levels in Lake Poyang. Thereby the water depth was mainly determined by lake's elevation and increased gradually from upstream to downstream. During low water level period, spatial difference of water level existed and water level decreased from lake's boundary to channel connected to Yangtze River. The distribution of water depth was not heterogeneous, excepting in narrow channel where water depth was higher than other lake zones. (3) Water velocity in Lake Poyang had series of characteristics, for instance, water velocity during high water level was slower than during lower water level period; the water velocity in narrow channel was significantly faster than in other region, excepting in high water level period. The water velocity in the northern zone was faster than southern area in majority of months. (4) The flow velocity was closely related to water level and different water level would drive different distribution of flow velocity. The water level and velocity simulation research laid a foundation for water management during dry period of large water bodies lately.

Key words: Lake Poyang, water level, water velocity, temporal and spatial distribution, EFDC

CLC Number: 

  • K292
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