4.5 Article

Assessment of drought trends and variabilities over the agriculture-dominated Marathwada Region, India

Journal

ENVIRONMENTAL MONITORING AND ASSESSMENT
Volume 194, Issue 12, Pages -

Publisher

SPRINGER
DOI: 10.1007/s10661-022-10532-8

Keywords

Meteorological drought; Marathwada; Drought trend; SPI; GLEAM; ESI

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Drought is a significant threat to the agriculture-dominated Marathwada Region in India, and the study highlights the importance of assessing drought trends and variabilities. The results show that the region is prone to droughts, with longer time frames capturing drought occurrences better. The study provides valuable information for devising water management strategies to minimize the repercussions of droughts in the monsoon-dominated region.
Drought is considered among the most perilous events with catastrophic consequences, particularly from the agro-economic point of view. These consequences are expected to exacerbate under the increasing meteorological aberrations due to changing climate, which necessitates investigating drought variabilities. This study presents a thorough spatiotemporal assessment of drought trends and variabilities over the agriculture-dominated Marathwada Region, Maharashtra, India. The precipitation data is extracted from the India Meteorological Department (IMD) gridded product, whereas actual evapotranspiration (ET) and Evaporative Stress Index (ESI) are obtained from Global Land Evaporation Amsterdam Model (GLEAM) datasets. Standardized Precipitation Index (SPI) is used to characterize drought occurrences at multiple time frames, whereas non-parametric tests, i.e., modified Mann-Kendall (MMK) and Sen's slope (SS) tests, are employed to detect trends. The results reveal the region to be prone to droughts, and SPI at a longer time frame (i.e., 12-monthly moving frame) can capture drought occurrences better than the shorter time frames, which can be attributed to the lesser randomness in the time series in the longer frame. A mix of positive/negative trends of SPI series are found for the monsoonal months; however, they are relatively more concentrated towards negative Z(MMK). Hence, the Marathwada Region can be inferred to have exhibited a relatively increased tendency towards drought occurrences. The seasonal differences in mean values and trends of rainfall, ET, and ESI are discussed in detail. Since the Marathwada Region has a monsoon-dominated climate with high agricultural importance, the information reported in this study will help in devising water management strategies to minimize the repercussions of droughts.

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