Tonle Sap Lake
The Mekong River system includes a physical marvel. During the wet season, the level of the Mekong River rises, backing up the Tonle Sap River and causing it to flow northwest into the Tonle Sap Lake.
Tonle Sap Lake expands from 2,500 square kilometres to 13,000/16,000 square kilometres, and its maximum depth increases from about 2.2 metres to more than 10 metres. In the dry season, the Great Lake reverses its flow and slowly drains into the Mekong River. This input helps control salinity intrusion and conserve mangrove forests in the Mekong’s Delta.
When the Tonle Sap and other parts of the Mekong system flood into fields and forests, fish take advantage of the huge increase in the availability of food. Some fish spawn in the main river channels and eggs and larvae drift into the flooded areas. Other species spawn in the flooded areas. As the floodwaters recede, fish retreat to main river channels.
Fish migrations from the Tonle Sap help restock fisheries as far upstream as China and in many tributaries along the way. There also is evidence that many species that are important parts of the subsistence and commercial fisheries in Tonle Sap spawn in other parts of the river system.