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008			150698 th eng
035			_a.b10583282
099		9	_aAIT Thesis no. WA-91-22
100	0		_aTruong Minh Chanh
245	1	0	_aSalinity intrusion in the Mekong estuarine system under the effect of sea level rise
260			_aBangkok : _bAsian Institute of Technology, _c1991
300			_a143 p.
490	1		_aThesis ; _vno. WA-91-22
500			_aA Thesis submitted in partial fulfillment of the requirement for the Degree of Master Engineering, School of Engineering and Technology
502			_aThesis (M.Eng.) - Asian Institute of Technology, 1991
520			_aThe effect of sea level rise on flow characteristics of the Lower Mekong Basin River has been detected under various magnitude orders of rising sea level and flow enter into the Mekong Delta with different scenarios due to the "Greenhouse Effect" during the dry season. These information are useful picture knew as a forecasting the variation of water level, freshwater discharge distribution and salinity intrusion along the Mekong River and Bassac River due to the changes of boundary conditions. In case of predicting of flow into the Mekong Delta under different scenarios, the General Circulation Models, i.e GISS, GFDL, UKMO models are used to produce the daily rainfall at six stations upper part of the Lower Mekong Basin, i.e Chiangrai, Luang Prabang, Vientiane, Nakon Phanom, Mukdahan and Pakse. The rainfall-runoff model developed for Pakse is applied to get the discharge at Pakse. The discharge at Kratie was found by suitable relationship between discharge at that station and that of at Pakse, Finally daily discharge at Phnompenh knew as flow enter the Mekong Delta, had been transferred from those of Kratie. The sea level rise scenarios could be extracted from various Research Institutes and Agencies, i. e the Environmental Protection Agency, National Center for Atmospheric Research. The Meksal Model is concentratedly used to yield the results for all cases of computation considering the two boundary conditions mentioned above. The results of computation convinciably give the good scene of forecast of the flow features of the Lower Mekong Basin River.
650		0	_aSea level
650		0	_aSaltwater encroachment _xMekong River
700	0		_aSuphat Vongvisessomjai, _eChairperson
700	1		_aGupta, Ashim Das, _eExamination Committee
700	1		_aShibayama, Tomoya, _eExamination Committee
710	2		_aThe Government of Germany, _eScholarship Donor
810	2		_aAsian Institute of Technology. _tThesis ; _vno. WA-91-22
856			_3Full-Text _uhttp://203.159.5.9/ait-thesis/detail.php?q=B17765
907			_a.b10583282 _bmnait _cs
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