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Climate change effect on water resources in Varanasi district, India

dc.contributor.authorNistor, Margarit-Mircea
dc.contributor.authorRai, Praveen K.
dc.contributor.authorDugesar, Vikas
dc.contributor.authorMishra, Varun N.
dc.contributor.authorSingh, Prafull
dc.contributor.authorArora, Aman
dc.contributor.authorKumra, Virendra Kumar
dc.contributor.authorCarebia, Iulius-Andrei
dc.date.accessioned2020-01-31T10:30:16Z
dc.date.available2020-01-31T10:30:16Z
dc.date.issued2019-12-23
dc.description.abstractEvapotranspiration and water availability are driven by changing climate and land cover parameters. In the present study, climatological records and land cover data were analysed simultaneously to accomplish the spatial distributions of climate change effects on water resources in Varanasi district, north India. Humidity–aridity was assessed by Lang's rain factor and De Martonne's aridity index, based on mean monthly rainfall and air temperature from seven meteorological stations. The climate change effect on water resources was evaluated using a 5 × 5 matrix that includes water availability and the aridity index by considering two time periods: 1941–1970 (1950s) and 1971–2000 (1980s). The methodology is based on seasonal crop evapotranspiration (ETc) (initial, mid-season, end season and cold season) and annual water availability calculations. The high values (≤ 1,045 mm) of ETc were identified during the mid-season stage. Water availability indicates decreases in the maximums from 718 to 636 mm during the two analysed periods, with a negative impact at the spatial scale. Lang's rain factor (< 40) indicates an arid climate in the northwest, west, east and central parts of the district and a humid climate (Lang's rain factor > 40) in the south. De Martonne's aridity index indicates rapid aridization from south to north (28.3 in the 1950s and 25.6 in the 1980s). The high and very high climate effects on water resources in Varanasi district were found mainly in the crop lands, while in the urban areas the climate effect is low. The much affected area by climate change and land cover was depicted during the recent period (1980s). This statement was proved also by the Mann and Kendall test, which indicates a negative trend for annual precipitation at all stations (for the period 1941–2000), while the mean annual temperature had a positive trend for four stations. These findings suggest that climate change had a negative effect on water resources during the last 60 years in the study area.en_US
dc.identifier.issn13504827
dc.identifier.urihttps://idr-sdlib.iitbhu.ac.in/handle/123456789/593
dc.language.isoenen_US
dc.publisherJohn Wiley and Sons Ltden_US
dc.subjectClimate changeen_US
dc.subjectClimate indicesen_US
dc.subjectEvapotranspirationen_US
dc.subjectLand Coveren_US
dc.subjectVaranasi districten_US
dc.subjectWater resourcesen_US
dc.titleClimate change effect on water resources in Varanasi district, Indiaen_US
dc.typeArticleen_US

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