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dc.contributor.advisorNanjundiah, Ravi S
dc.contributor.authorJanakiraman, S
dc.date.accessioned2026-03-11T07:21:54Z
dc.date.available2026-03-11T07:21:54Z
dc.date.submitted1998
dc.identifier.urihttps://etd.iisc.ac.in/handle/2005/9152
dc.description.abstractThe mass continuity equation traditionally used in atmospheric models does not take into account the local sources and sinks. The mass of the atmosphere varies due to the moisture variation arising from evaporation and precipitation. Evaporation and precipitation are the local sources and sinks of atmospheric mass. So far, almost all models do not include this effect of moisture variation on atmospheric mass and instead only adjust the virtual temperature. This leads to an inconsistency in the model formulation. In the present study, we have incorporated the effect of moisture variation into the mass budget equation of the NCAR CCM2 General Circulation Model. This is called Water Mass Forcing (WMF). The present study is exploratory in nature. We have found that WMF has significantly modified the climate of the tropics. In particular, the precipitation and wind simulations for the Indian summer monsoon have improved substantially
dc.language.isoen_US
dc.relation.ispartofseriesT04438
dc.rightsI grant Indian Institute of Science the right to archive and to make available my thesis or dissertation in whole or in part in all forms of media, now hereafter known. I retain all proprietary rights, such as patent rights. I also retain the right to use in future works (such as articles or books) all or part of this thesis or dissertation
dc.subjectWater Mass Forcing
dc.subjectMesoscale modeling
dc.subjectGeneral Circulation Model
dc.titleImpact of water mass forcing on the general circulation model simulations
dc.typeThesis
dc.degree.nameMsc Engg
dc.degree.levelMasters
dc.degree.grantorIndian Institute of Science
dc.degree.disciplineScience


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