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Outflow lake

[wài liú hú]
Some lakes connect with rivers and finally flow into the ocean
Drain the lake refers to a lake whose water is connected with rivers and finally flows into the sea. Outflow river Along the main rivers and tributaries of the Yangtze River, the climate is relatively mild and humid, the precipitation is rich, and the river supply is mainly rainwater. In addition, the river water volume is abundant, so the lake water level is obviously affected by river regime Generally, the annual change process of the two is closely consistent. [1]
Chinese name
Outflow lake
Foreign name
Drain the lake
Introduction
The lake is connected with the river and finally flows into the ocean
Features
yes River runoff It has obvious regulating effect
Climatic environment
The coastal climate is mild and humid, with abundant rainfall
Distribution in China
Northeast, East, South and Southwest China

interpretation

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A lake whose water connects with rivers and finally flows into the ocean. Along the main and tributaries of the outflow river, the climate is relatively mild and humid, the precipitation is rich, and the river supply is mainly rain. In addition, the river water volume is abundant, which has a large amount of supply to lakes. The lake water level is obviously controlled by the river water regime, and the change process of the two is usually closely consistent within the year. The water balance of the outflow lake is characterized by: the supply part is mainly from the inflow runoff, the loss part is mainly from the outflow runoff, and the proportion of precipitation, evaporation and leakage on the lake surface is small. The lake has an obvious regulating effect on the river runoff, making the water level of the downstream river change relatively gently, and the flood peak lags behind. [2]

Characteristics and distribution

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characteristic

Outflowing lacustrine Water balance The characteristics are: the supply is mainly from the lake runoff The loss is mainly the runoff from the lake, and the proportion of precipitation, evaporation and leakage on the lake surface is small. Lake pair River runoff It has obvious regulation effect, so that the water level of the downstream river changes relatively gently and the flood peak lags behind. The highest water level of the outflow lake is mostly in the rainy season, usually in August and September, and the lowest water level is mostly in the season with little rain or the most water.

distribution

The outflow lakes in China are mainly distributed in northeast, east, south and southwest China. Mainly refers to Greater Khingan Range - Hell Mountain - Helan Mountain Qilian Mountains - Kunlun Mountain - Tanggula Mountain - Gangdise Mountain The outflow lake area in the southeast of the first line. as Poyang Lake Dongting Lake , Zhaling Lake Eling Lake Etc.