Abstract

Abstract. The vulnerability and trends of meteorological as well as agricultural drought conditions over Indian region was studied using long-term (1982–2015) gridded precipitation and time-series normalized difference vegetation index (NDVI) data. The Climate Hazards Group Infra-Red Precipitation with Station (CHIRPS) precipitation data (~5 km) was used to compute Standardized precipitation index (SPI) at 3-month time scale for Indian summer monsoon season (June-September). Subsequently, the long-term Global Inventory Modelling and Mapping Studies (GIMMS) time-series NDVI data (~8 km) was interpolated at daily scale and smoothened using Savitzky and Golay filtering method. Further, the time-series NDVI data was transformed into several phenological parameters using threshold and derivative approach. As integrated NDVI, i.e. the area under seasonal NDVI curve, is able to represent the anomalies in seasonal agricultural production, it was transformed into standardized vegetation index (SVI) using empirical distribution. Several drought parameters, e.g. magnitude and extent, were computed at district level based on the SPI and SVI values, where values with SPI or SVI less than minus one was considered as meteorological and agricultural drought year, respectively. The trends of drought magnitude and extent for both the meteorological and agricultural drought were estimated using Sen’s slope. The direction of trends and magnitude were found to be varying spatially across different parts of Indian region. Further, the mean SPI/SVI values along with drought frequency were utilized to categorize entire Indian agricultural area into different vulnerable zones during three decades separately. The overall drought vulnerability was found to be decreasing over time.

Highlights

  • Drought is a climatic phenomenon that affects the natural variability of the climate system

  • In the case of standardized vegetation index, the mean SVI values were very high in the western region of India

  • The meteorological drought frequency was very high over western India during first decade of the study period, whereas in two decades, i.e. 1993-2002 and 2003-2015, it was found to be decreasing

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Summary

Introduction

Drought is a climatic phenomenon that affects the natural variability of the climate system. Droughts are slow-onset phenomenon; especially extensive event of nature which can affect a region for weeks, months or may be years. Because of this creeping phenomenon, drought can be the cause of prompting mass migration, environmental degradation and famine-like situation (Rojas et al 2011). One of the most popular perceptions of drought is meteorological drought phenomenon. This kind of phenomenon can be occurred due to lack of expected precipitation. South-west monsoon from June to September is the reason, that India receives more than 70% rainfall every year (Mishra et al, 2010)

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