Abstract

Drought is a complex natural hazard which can have negative effects on agriculture, economy, and human life. In this paper, the primary goal is to explore the application of the Gravity Recovery and Climate Experiment (GRACE) gravity satellite data for the quantitative investigation of the recent drought dynamic over the arid land of northwestern China, a region with scarce hydrological and meteorological observation datasets. The spatiotemporal characteristics of terrestrial water storage changes (TWSC) were first evaluated based on the GRACE satellite data, and then validated against hydrological model simulations and precipitation data. A drought index, the total storage deficit index (TSDI), was derived on the basis of GRACE-recovered TWSC. The spatiotemporal distributions of drought events from 2003 to 2012 in the study region were obtained using the GRACE-derived TSDI. Results derived from TSDI time series indicated that, apart from four short-term (three months) drought events, the study region experienced a severe long-term drought from May 2008 to December 2009. As shown in the spatial distribution of TSDI-derived drought conditions, this long-term drought mainly concentrated in the northwestern area of the entire region, where the terrestrial water storage was in heavy deficit. These drought characteristics, which were detected by TSDI, were consistent with local news reports and other researchers’ results. Furthermore, a comparison between TSDI and Standardized Precipitation Index (SPI) implied that GRACE TSDI was a more reliable integrated drought indicator (monitoring agricultural and hydrological drought) in terms of considering total terrestrial water storages for large regions. The GRACE-derived TSDI can therefore be used to characterize and monitor large-scale droughts in the arid regions, being of special value for areas with scarce observations.

Highlights

  • Drought, as a complex natural hazard, develops slowly but can last for months or even years, and possibly causes more serious harm compared with other natural disasters.Drought seriously damages agricultural production, ecosystems, and economic and social conditions [1].In recent years, global climate change had a direct effect on the frequency and intensity of extreme drought events in many regions across the world, especially in semi-arid areas such as northwesternChina [2]

  • Prior to calculating the total storage deficit index (TSDI) index, the Gravity Recovery and Climate Experiment (GRACE) terrestrial water storage changes (TWSC) need to be validated to ensure their accuracy within the target region

  • The GRACE TWSC were compared with hydrological models TWSC and precipitation

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Summary

Introduction

As a complex natural hazard, develops slowly but can last for months or even years, and possibly causes more serious harm compared with other natural disasters (e.g., earthquakes and floods).Drought seriously damages agricultural production, ecosystems, and economic and social conditions [1].In recent years, global climate change had a direct effect on the frequency and intensity of extreme drought events in many regions across the world, especially in semi-arid areas such as northwesternChina [2]. Global climate change had a direct effect on the frequency and intensity of extreme drought events in many regions across the world, especially in semi-arid areas such as northwestern. During the first decade of the 21st century, China suffered from a series of severe droughts [3]. In China, the annual average crop area that suffered from drought was of 62.0 million acres in the beginning of this century, in comparison to 28.7 million acres in the 1950s [4]. The annual average grain production loss rose to 34.9 million tons in the first decade of the 21st century, a loss which is 703% larger compared to that in the 1950s [4]. Reported direct economic losses from droughts were over 16 billion USD in 2009 in China [5]. In the face of increasingly severe droughts, it is urgent to take effective measures to continuously monitor this phenomenon

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