Climate indices and drought characteristics in the river catchments of Western Ghats of India

dc.contributor.authorShetty, S.
dc.contributor.authorUmesh, P.
dc.contributor.authorShetty, A.
dc.date.accessioned2026-02-04T12:25:16Z
dc.date.issued2024
dc.description.abstractThe study addresses the long-term trend in rainfall, minimum and maximum temperature, and the climate indices for the river catchments located in the diverse climate of the Western Ghats of India. The dry sub-humid Chaliyar catchment and humid Kajvi catchment have shown a dramatic change in the decadal rainfall, with the decade 1950–1960 being the point of change. The monsoon rainfall has decreased in the Chaliyar and Netravati catchments and increased insignificantly in the Kajvi catchment. With the increase in mean temperature, the number of rainy days is decreasing, and intense rainfall is increasing in the pre-monsoon. The increase in minimum temperature is more severe in all three catchments, irrespective of the region’s climate. The decline in rainy days is more figurative in the humid and per-humid catchments and has seen a 16–20% decrease in R×1 day, R×3 day, and R×5 day in the past six decades with an insignificant increase in the dry sub-humid catchment. The frightful increase in warm days/nights with a decrease in cool days/nights has been alarming for the extremity of temperature in future years. The significant changes in the forest area in Chaliyar and Kajvi catchment and the increase in a built-up area in Netravati may have a decisive role in the nonseasonal variability in rainfall and temperature along with increasing greenhouse gases. In the case of meteorological drought studied using the Standardized Precipitation Index (SPI), moderate droughts have occurred over the Chaliyar and Kajvi, and extreme droughts over the Netravati catchments with no reduction in the frequency or severity of short-duration extreme rainfall events. The geographical location of the catchment has a greater impact on the characteristics of the rainfall and meteorological drought, and these changes in the hydrological regimes of the catchment have a significant bearing on the water availability in the catchments in the future years. © The Author(s) under exclusive licence to Institute of Geophysics, Polish Academy of Sciences & Polish Academy of Sciences 2023.
dc.identifier.citationActa Geophysica, 2024, 72, 1, pp. 371-384
dc.identifier.issn18956572
dc.identifier.urihttps://doi.org/10.1007/s11600-023-01054-z
dc.identifier.urihttps://idr.nitk.ac.in/handle/123456789/21318
dc.publisherSpringer Science and Business Media Deutschland GmbH
dc.subjectAtmospheric thermodynamics
dc.subjectDrought
dc.subjectForestry
dc.subjectGreenhouse gases
dc.subjectRain
dc.subjectRunoff
dc.subject'Dry' [
dc.subjectClimate index
dc.subjectClimate variability
dc.subjectDrought characteristics
dc.subjectMeteorological drought
dc.subjectMinimum temperatures
dc.subjectRainy days
dc.subjectRiver catchment
dc.subjectSub-humid
dc.subjectWestern ghats
dc.subjectCatchments
dc.subjectcatchment
dc.subjectclimate variation
dc.subjectdrought
dc.subjectprecipitation intensity
dc.subjecttemperature anomaly
dc.subjecttrend analysis
dc.subjectIndia
dc.subjectWestern Ghats
dc.titleClimate indices and drought characteristics in the river catchments of Western Ghats of India

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