Through inputting known parameters,we found that once the Coriolis force combined with the stratification of the lake,it not only determined the direction of the river water,but also seemed to affect greatly the steady state pattern of the flow.
通过输入已知参数结果表明:纳木错湖周边山水(河水)流入湖泊之后,在柯氏力[2]和湖水分层[3]的影响下,所有流入湖泊的河水沿着湖岸呈逆时针方向循环流动;循环周期约需要60天左右;河水首尾相连后继续沿着湖岸按逆时针方向均匀流动且朝着湖心聚集;河水在湖中的水平分布不仅受柯氏力的影响同时也受湖水分层的影响。
