Analysis of climate trend and effect of land use land cover change on Harangi streamflow, South India: a case study

dc.contributor.authorAnil, A.P.
dc.contributor.authorRamesh, H.
dc.date.accessioned2026-02-05T09:32:07Z
dc.date.issued2017
dc.description.abstractLand use land cover (LULC) and climate change are considered to be driving factors contributing to the alteration of the hydrological regime. Therefore, an attempt has been made to study climate trend and the effect of LULC on streamflow in a basin covered predominantly by forest. The Harangi river basin is one of such basins located in the western ghats of South India. The LULC trend was carried out by considering temporal multispectral data for the years 1990, 2002 and 2008 obtained from Landsat-5TM and IRS 1C (Indian Remote Sensing Satellites). Climate parameters such as rainfall and temperatures were considered for the trend analysis in this study. The rainfall trend was studied using Man-Kendall and Sen’s slope method to understand the spatio-temporal variability. Rainfall shows the decrease trend at Suntikoppa rain gauge station in January and June months. Harangi and Madapura rain gauge stations also show a decrease of rainfall trend for only January month. Temperature trend show increase in maximum temperature for the month of April, May and November whereas increase in minimum temperature was observed in the month of November and December. Spatial extent of LULC found that 52.4% (220.014 km2) of the study area was covered with forest in 1990 which has considerably decreased to 43.9% (184.53 km2) in 2008. There was a rise in total area of plantation crops from 106.27 km2 (25.32%) to 138.20 km2 (32.9%) during this period. Soil and Water Assessment Tool (SWAT) was used to study the effect of LULC on streamflow. SWAT model was calibrated and validated using observed daily streamflow data. The coefficient of correlation (r2) was found to be 0.87 and 0.86 for calibration and validation, respectively. The results found the annual streamflow to increase by 0.77% from 1990 to 2008 whereas the mean monthly streamflow has increased by 9.46% during this period. This was mainly due to the reduction in forest area observed in LULC maps. © 2017, Springer International Publishing Switzerland.
dc.identifier.citationSustainable Water Resources Management, 2017, 3, 3, pp. 257-267
dc.identifier.issn23635037
dc.identifier.urihttps://doi.org/10.1007/s40899-017-0088-5
dc.identifier.urihttps://idr.nitk.ac.in/handle/123456789/25509
dc.publisherSpringer Science and Business Media Deutschland GmbH
dc.subjectForestry
dc.subjectLand use
dc.subjectRain
dc.subjectRain gages
dc.subjectRemote sensing
dc.subjectStream flow
dc.subjectCalibration and validations
dc.subjectCoefficient of correlation
dc.subjectIndian remote sensing satellite
dc.subjectLand use land cover change
dc.subjectLand use/ land covers
dc.subjectMinimum temperatures
dc.subjectSoil and water assessment tool
dc.subjectSpatiotemporal variability
dc.subjectClimate change
dc.subjectclimate change
dc.subjectclimate effect
dc.subjecthigh temperature
dc.subjecthydrological regime
dc.subjecthydrological response
dc.subjectland cover
dc.subjectland use change
dc.subjectmodel test
dc.subjectmodel validation
dc.subjectriver basin
dc.subjectstreamflow
dc.subjectHarangi Basin
dc.subjectIndia
dc.titleAnalysis of climate trend and effect of land use land cover change on Harangi streamflow, South India: a case study

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