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Both drought and flood are widespread hazards in the Delta, which many people imagine is essentially the most sensitive to upstream hydrological change. Reach 1: Lancang Jiang or Upper Mekong River in China. On this part of the river, the main supply of water flowing into the river comes from melting snow on the Tibetan plateau. This quantity of water is generally known as the "Yunnan part" and plays an necessary function in the low-circulate hydrology of the decrease mainstream. At the same time as far downstream as Kratie, the Yunnan component makes up almost 30% of the average dry season flow. A serious concern is that the continued and deliberate growth of dams and reservoirs on the Mekong mainstream in Yunnan could have a big effect on the low-flow regime of the decrease Mekong basin system. Reach 2: Chiang Saen to Vientiane and Nong Khai. This reach is nearly totally mountainous and covered with pure forest though there was widespread slash and burn agriculture. Although this attain cannot be termed "unspoiled", the hydrological response is probably probably the most natural and undisturbed of all the lower basin. Many hydrological features of the lower basin start to vary quickly at the downstream boundary of this reach. On 19 July 2019 this reach of the river dropped to its lowest degree in a century. Officials are notably involved as July is in the wet season, when mainstream flows are considerable historically. Reach 3: Vientiane and Nong Khai to Pakse. The boundary between Reach 2 and three is where the Mekong hydrology starts to alter.