Tonlé Sap – the lake whose river reverses twice a year

Tonlé Sap

86%
Flow reversed, lake filling
Estimated area 13,275 km² · Estimated depth 8.3 m

The Mekong now stands higher than the lake, so the Tonlé Sap river runs backwards and pumps water in. Fish move upstream into the lake to spawn. This is when the lake expands fastest.

Mekong basin rainfall: 39 mm over the past 72 hours, 30 mm forecast for the next 72.

This is a seasonal estimate combined with basin rainfall, not a measured level. Official water level and discharge come from the Mekong River Commission (MRC). The timing of the reversal varies year to year and has shifted noticeably over the past two decades.

Why the lake reverses

The annual cycle

MonthStateAreaDepth
JanuaryFlow reversed again, lake draining5,813 km²3.3 m
FebruaryFlow reversed again, lake draining4,844 km²2.6 m
MarchFlow reversed again, lake draining3,969 km²2 m
AprilFlow reversed again, lake draining3,000 km²1.3 m
MayDry season, lake contracting3,083 km²1.4 m
JuneFlow reversed, lake filling4,375 km²2.3 m
JulyFlow reversed, lake filling7,099 km²4.1 m
AugustFlow reversed, lake filling9,915 km²6 m
SeptemberFlow reversed, lake filling12,730 km²8 m
OctoberLake at maximum extent14,880 km²9.4 m
NovemberFlow reversed again, lake draining13,059 km²8.2 m
DecemberFlow reversed again, lake draining9,112 km²5.5 m

Why the river reverses

The Tonlé Sap river links the lake to the Mekong at Phnom Penh. Its direction is set by the difference in water level, not by terrain. In the dry season the lake stands higher and drains out. In the wet season, snowmelt from the Tibetan plateau plus the monsoon raise the Mekong until it exceeds the lake, and the flow reverses inward. The lake works as a natural relief valve for the lower Mekong, absorbing the flood peak and releasing it slowly.

Why this decides what the country eats

As the lake rises it submerges roughly a million hectares of flooded forest around its edge. That forest is where fish spawn and fry grow. Cambodia's freshwater catch depends almost entirely on whether the lake rises high enough for long enough. Fish is the main protein source for most of the population, so a weak flood year is a protein shortage, not only an income shortage.

What is changing

The timing and amplitude of the flood have shifted noticeably over two decades. The reasons most often cited are the chain of upstream Mekong dams together with a more erratic monsoon. That is why this page estimates from actual basin rainfall rather than a fixed date — a fixed calendar would drift further wrong each year.

If you are visiting

September to November is when the lake is widest: the floating villages of Kampong Phluk and Chong Kneas are easy to reach by boat and the Prek Toal flooded forest is fully submerged. March to May the lake is low, many boat channels are unusable and the floating villages sit on mud. Bon Om Touk, around early November, marks the moment the flow turns back out.

Provinces around the lake