Abstract

Assessing the impacts of human activities on the variations in terrestrial water storage (TWS) is essential for water resource management, particularly in regions like the Aral Sea Basin which suffers from severe water scarcity. In this study, the variations in TWS anomalies (TWSA) of the Aral Sea Basin during the period of April 2002 to June 2017 were analyzed using Gravity Recovery and Climate Experiment (GRACE) data and the Global Land Data Assimilation System (GLDAS) Noah model outputs. The impacts of human activities on TWS variations were further quantified through the variations in TWS components and the comparison of TWS obtained from GRACE and GLDAS. The results indicate that TWSA of the entire Aral Sea Basin derived from GRACE experienced a significant decreasing trend of 4.12 ± 1.79 mm/year (7.07 ± 3.07 km3/year) from 2002 to 2017. Trends in individual TWS components indicate that the reduction in TWS of the Aral Sea Basin was primarily attributed to surface water loss, followed by groundwater depletion, which account for ~53.16% and 11.65 ± 45.39 to 42.48 ± 54.61% of the total loss of TWS, respectively. Precipitation (P) and evapotranspiration (ET) both exhibited increasing trends, indicating that ET played a dominant role in TWS depletion from the perspective of water balance. The variations in ET and TWS induced by human activities contributed ~45.54% and ~75.24% to those in total ET and TWS of the Aral Sea Basin, respectively.

Highlights

  • Terrestrial water storage (TWS) is an essential component of the terrestrial and global hydrological cycles, which mainly comprises surface water, groundwater, soil moisture, plant canopy water, snow, and glaciers [1,2,3]

  • Since Global Land Data Assimilation System (GLDAS) TWS anomalies (TWSA) only reflects the variations in three elements of Gravity Recovery and Climate Experiment (GRACE) TWSA, these findings suggest that the variations in soil moisture, snow water equivalent, and plant canopy water account for a small proportion (~19.66%) of total TWS

  • The temporal and spatial variations in TWS of the Aral Sea Basin during the period of April 2002 to June 2017 were investigated by using GRACE data and GLDAS

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Summary

Introduction

Terrestrial water storage (TWS) is an essential component of the terrestrial and global hydrological cycles, which mainly comprises surface water (lakes, rivers, and reservoirs), groundwater, soil moisture, plant canopy water, snow, and glaciers [1,2,3]. Due to the scarcity of water resources in arid and semi-arid regions, these components of TWS, surface water and groundwater, become of great ecological and social importance [4,5]. Global warming has exacerbated the variability of TWS in arid and semiarid regions, intensified further by human activities such as agricultural irrigation [6,7]. The Aral Sea Basin, an endorheic basin located in arid Central Asia, suffers from severe water scarcity under the influence of human activities [8,9,10]. With the rapid increase in water withdrawal since the 1960s, especially for damming and irrigation, the eco-environment dominated by water in the Aral Sea Basin has been deteriorating [4,11,12,13]

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