Publication:
Influences of land use and climate changes on hydrologic system in the northeastern river basin of Thailand

dc.contributor.authorNuanchan Singkranen_US
dc.contributor.authorJaruporn Tosangen_US
dc.contributor.authorDoungjai Waijaroenen_US
dc.contributor.authorNaree Intharawichianen_US
dc.contributor.authorOrnanong Vannararten_US
dc.contributor.authorPitchaya Anantawongen_US
dc.contributor.authorKarika Kuntaen_US
dc.contributor.authorPoonsak Wisetsopaen_US
dc.contributor.authorTanomkwan Tipvongen_US
dc.contributor.authorNaruekamon Janjirawuttikulen_US
dc.contributor.authorFatah Masthaweeen_US
dc.contributor.authorSanguanpran Amornpatanawaten_US
dc.contributor.authorSukrit Kirtsaengen_US
dc.contributor.otherMahidol Universityen_US
dc.contributor.otherThailand Land Development Department, Bangkoken_US
dc.contributor.otherDepartment of Water Resourcesen_US
dc.contributor.otherMekong River Commissionen_US
dc.contributor.otherPollution Control Departmenten_US
dc.contributor.otherThai Meteorological Departmenten_US
dc.date.accessioned2018-11-23T10:04:22Z
dc.date.available2018-11-23T10:04:22Z
dc.date.issued2015-01-01en_US
dc.description.abstract© IWA Publishing 2015. This study was a first attempt to portray the effects of land use and climate changes (CCs) on the hydrologic system in the Lamtakhong Basin in northeastern Thailand, which has been disturbed by various human activities, making it difficult to determine these impacts on hydrologic conditions. The hydrologic Soil and Water Assessment Tool model was set up with land use and soil data of 2002 and observed flow and weather data during 1999–2000. After the model was calibrated and validated against observed flow data during 2001–2009, its land use change scenario with input land use data of 2011 and its CC scenario with input weather data during 2010–2065 were simulated. The results showed that changing land use over the 10-year period had trivial influences on the hydrologic system, whereas changing climate over the 56-year period appeared to affect both water yields and flows. Water scarcity will tend to take place across the Lamtakhong Basin in the near future. Longer periods of severe droughts and floods might occasionally occur, particularly downstream. These findings will be useful for land and water resources managers and policy-makers to manage land and water resources in the river basin.en_US
dc.identifier.citationJournal of Water and Climate Change. Vol.6, No.2 (2015), 325-340en_US
dc.identifier.doi10.2166/wcc.2014.127en_US
dc.identifier.issn20402244en_US
dc.identifier.other2-s2.0-84930744391en_US
dc.identifier.urihttps://repository.li.mahidol.ac.th/handle/20.500.14594/35890
dc.rightsMahidol Universityen_US
dc.rights.holderSCOPUSen_US
dc.source.urihttps://www.scopus.com/inward/record.uri?partnerID=HzOxMe3b&scp=84930744391&origin=inwarden_US
dc.subjectEarth and Planetary Sciencesen_US
dc.subjectEnvironmental Scienceen_US
dc.titleInfluences of land use and climate changes on hydrologic system in the northeastern river basin of Thailanden_US
dc.typeArticleen_US
dspace.entity.typePublication
mu.datasource.scopushttps://www.scopus.com/inward/record.uri?partnerID=HzOxMe3b&scp=84930744391&origin=inwarden_US

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