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Mekong Floods Fill Tônlé Sap
This page contains archived content and is no longer being updated. At the time of publication, it represented the best available science. However, more recent observations and studies may have rendered some content obsolete.
The monsoon season in Southeast Asia brings recurring, often devastating floods to countries in the region, but these floods also play a necessary role in the regions water cycle. These MODIS images centered on Cambodia reveal extensive flooding of the Mekong River, which comes in from Laos in the north, to the right of center in the images, and flows south through Cambodia and southeast through Vietnam to empty into the South China Sea. The true-color image shows the brownish, sediment-laden floodwaters filling the Mekong Delta in southern Cambodia and Vietnam on September 15, 2001. The false color image above has been enhanced to bring out the contrast between the floodwaters and the lands, with sediment-carrying floodwaters in purple. Sediment can be seen flowing into the South China Sea as well. This years floods have affected over a million people, and 100 people have been killed in Vietnam alone.
The monsoon floods bring not only devastation, but renewal. The large body of water just left of center in Cambodia is the T“nl‚ Sap. This shallow lake plays a changing role in the regional water cycle. During the dry season, the stream-fed T“nl‚ Sap drains via the T“nl‚ Sab River into the Mekong River. During the wet season (June-November), flooding of the Mekong reverses the course of the T“nl‚ Sab, roughly tripling the lakes size from about 3000 km2 to about 10,000. When the dry season returns, the lake once again begins to drain into the Mekong Delta, where it provides a flow of fresh water that balances the intrusion of salty seawater into the deltas agricultural lands.
Image courtesy Jacques Descloitres, MODIS Land Rapid Response Team at NASA GSFC