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The first group are left bank tributaries that drain the excessive rainfall areas of Laos. The second group are those on the fitting bank, primarily the Mun and Chi Rivers, that drain a big part of northeast Thailand. Laos lies almost fully throughout the lower Mekong basin. Its climate, panorama and land use are the key components shaping the hydrology of the river. The mountainous panorama implies that only 16% of the nation is farmed underneath lowland terrace or upland shifting cultivation. With upland shifting agriculture (slash and burn), soils get better inside 10 to 20 years but the vegetation does not. Shifting cultivation is common in the uplands of northern Laos and is reported to account for as much as 27% of the full land underneath rice cultivation. As elsewhere in the basin, forest cover has been steadily diminished in the course of the final three a long time by shifting agriculture and everlasting agriculture. The cumulative impacts of these actions on the river regime have not been measured. However, the hydrological impacts of land cowl adjustments induced by the Vietnam War had been quantified in two sub-catchments of the lower Mekong River basin. Loss of forest cowl in the Thai areas of the decrease basin has been the best anti stretch mark cream after pregnancy of all of the decrease Mekong nations over the previous 60 years. Although this a part of northeast Thailand has an annual rainfall of greater than 1,000 mm (forty in), a high evaporation fee means it is categorised as a semi-arid area. Consequently, although the Mun and Chi basins drain 15% of your complete Mekong basin, they solely contribute 6% of the average annual circulation.

Sandy and saline soils are the most common soil sorts, which makes much of the land unsuitable for wet rice cultivation. In spite of poor fertility, nevertheless, agriculture is intensive. Glutinous rice, maize, and cassava are the principal crops. Drought is by far the most important hydrological hazard in this region. As the Mekong enters Cambodia, over 95% of its flows have already joined the river. From here on downstream the terrain is flat and water levels fairly than move volumes decide the motion of water across the landscape. The seasonal cycle of fixing water ranges at Phnom Penh results within the distinctive "flow reversal" of water into and out of the great Lake via the Tonle Sap River. Phnom Penh also marks the start of the delta system of the Mekong River. Here the mainstream begins to interrupt up into an increasing number of branches. In Cambodia, wet rice is the main crop and is grown on the flood plains of the Tonle Sap, Mekong, and Bassac (the Mekong delta distributary known because the Hậu in Vietnam) Rivers. Here, the river panorama is flat. Small adjustments in water degree decide the route of water movement, together with the big-scale reversal of move into and out of the Tonle Sap basin from the Mekong River. The Mekong Delta in Vietnam is farmed intensively and has little natural vegetation left. Forest cover is less than 10%. In the Central Highlands of Vietnam, forest cover was lowered from over 95% in the 1950s to around 50% within the mid-nineties. Agricultural growth and population stress are the foremost causes for land use and landscape change.

Both drought and flood are widespread hazards within the Delta, which many individuals consider is the most sensitive to upstream hydrological change. Reach 1: Lancang Jiang or Upper Mekong River in China. In this part of the river, the foremost source of water flowing into the river comes from melting snow on the Tibetan plateau. This volume of water is typically known as the "Yunnan part" and plays an necessary position in the low-stream hydrology of the lower mainstream. Even as far downstream as Kratie, the Yunnan component makes up almost 30% of the average dry season movement. A major concern is that the continued and deliberate enlargement of dams and reservoirs on the Mekong mainstream in Yunnan could have a big impact on the low-stream regime of the decrease Mekong basin system. Reach 2: Chiang Saen to Vientiane and Nong Khai. This reach is nearly solely mountainous and coated with natural forest though there was widespread slash and burn agriculture. Although this reach can't be termed "unspoiled", the hydrological response is probably probably the most natural and undisturbed of all of the decrease basin. Many hydrological elements of the lower basin start to change rapidly at the downstream boundary of this attain. On 19 July 2019 this attain of the river dropped to its lowest level in a century. Officials are particularly concerned as July is within the wet season, when mainstream flows are considerable traditionally. Reach 3: Vientiane and Nong Khai to Pakse. The boundary between Reach 2 and 3 is where the Mekong hydrology begins to alter.