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日本琵琶湖的水动力三维数值模拟
引用本文:张利民,濮培民.日本琵琶湖的水动力三维数值模拟[J].海洋与湖沼,1996,27(1):86-92.
作者姓名:张利民  濮培民
作者单位:中科院南京地理与湖泊研究所!南京210008
摘    要:在笛卡尔坐标下,运用流体水动力学的方法,并在前人观测资料的基础上建立了一个三维水动力数值模式,并对日本琵琶湖风生流进行了数值模拟。结果表明,在5m/s的东南风、西南风、东北风作用下,湖的北端均有气旋式环流出现,在5m/s西北风作用下,湖的北端有反气旋式环流出现。在各种方向风速驱动下,中、低层场或形成与表层一致的环流型,或呈现明显的垂直切变。

关 键 词:琵琶湖  水动力  数值模拟  湖泊
收稿时间:1993/6/19 0:00:00
修稿时间:1993/8/13 0:00:00

A MULTI-LEVEL MODEL OF HYDRODYNAMICS OF THE LAKE BIWA IN JAPAN
Zhang Limin and Pu Peimin.A MULTI-LEVEL MODEL OF HYDRODYNAMICS OF THE LAKE BIWA IN JAPAN[J].Oceanologia Et Limnologia Sinica,1996,27(1):86-92.
Authors:Zhang Limin and Pu Peimin
Institution:Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing 210008;Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing 210008
Abstract:On the basis of former works, a three dimensional numerical model ofthe lake hydrodynamics was designed to simulate the wind - driven current in thisstudy to address the pollutants diffosion, sediment transport, and recentlyworsening water quality of Lake Biwa, Japan. The study results show, the forcingaction of uniform 5m/s SE, SW, NE winds cause an anticlockwise circulation inthe north of the North Basin, but a clockwise circulation in the case of 5m/s NWwind. But the Gyres, currents opposite to those at the surface layer are formed atthe middle and lower layers.
Keywords:Lake Biwa  Hydrodynamics  Numerical model
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