Impact of climate change on hydrology of Manjalar sub basin of river Vaigai in Tamil Nadu, India

This study evaluates the impacts of possible future climate change scenarios on the hydrology of the catchment area of the Manjalar sub basin of River Vaigai, Tamil Nadu, India carried out at the department of Soil and Water Conservation Engineering, Tamil Nadu Agricultural University during the per...

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Bibliographic Details
Published in:Journal of applied and natural science 2016-09, Vol.8 (3), p.1670-1679
Main Authors: Janapriya, S., Bosu, S. Santhana, Kannan, Balaji
Format: Article
Language:English
Subjects:
21st century
Agricultural engineering
Annual rainfall
Catchment areas
Climate change
Climate models
Evapotranspiration
Groundwater
Hydrologic models
Hydrology
Moisture content
Rainfall
Rivers
Soil conservation
Soil water
Soil water storage
Stream discharge
Stream flow
Surface runoff
Water conservation
Water resources
Water storage
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Summary:This study evaluates the impacts of possible future climate change scenarios on the hydrology of the catchment area of the Manjalar sub basin of River Vaigai, Tamil Nadu, India carried out at the department of Soil and Water Conservation Engineering, Tamil Nadu Agricultural University during the period of 2011-2014 using Soiland Water Assessment Tool (SWAT). For the climate impact assessment the hydrological model was driven with output of bias corrected Earth System Models of the Coupled Model Intercomparison Project Phase 5 (CMIP5): HadGEM2. Climate scenarios were downscaled to a grid resolution of 0.22° x 0.22°. In this study RCP 4.5 and RCP 8.5 were included for future assessment with three future periods: 2012–2039, 2040–2069, and 2070–2098. The projected increase in maximum and minimum temperature for RCP 4.5 scenario is 0.8 to 2.3 ºC and 0.7 to 1.6 ºC and for RCP 8.5 scenario is 1.1 to 4.0 ºC and 1.0 to 3.1 ºC, respectively. Rainfall is projected to an increase between 9.2 to 15.2 per cent for RCP 4.5 scenario and an increase of 13.6 to 18.8 per cent for RCP 8.5 scenario during 21st century. The soil water storage and stream flow contribution to ground water are likely to increase in RCP 4.5 scenario and it would again decline for RCP 8.5 scenario during 21st century. The increase in annual rainfall evapotranspiration and surface runoff would be more in RCP 8.5 scenario compared to RCP 4.5 scenario. The possible changes projected by the study provide a useful input to effective planning of water resources of the study area.
ISSN:0974-9411
2231-5209
DOI:10.31018/jans.v8i3.1021