The impact of climate change and human activities on the Aral Sea Basin over the past 50 years
Introduction
Lakes play a significant role in maintaining the survival and development of human habitations and the stability of the surrounding ecology, especially in arid regions with fragile environments (Klein et al., 2014). The Aral Sea is a typical inland lake located in the Central Asia. Over the past 50 years, the lake has experienced a sharp reduction in water, which has produced serious negative effects on water resources and the local ecology. This phenomenon grabbed world-wide attention in the 1990s and has since been dubbed “the Aral Sea crisis” (Chen et al., 2018; Micklin, 2016).
The Aral Sea Basin includes five Central Asian countries (Kazakhstan, Kyrgyzstan, Tajikistan, Turkmenistan and Uzbekistan) as well as Afghanistan and Iran. Overall, the five Central Asian countries are the main water-consumers in the basin, as the economies of these countries depend mainly on irrigated agriculture (Awan et al., 2011). Since 1960, a large-scale reclamation and irrigation of the Soviet Union and post-Soviet Union countries have consumed an immense amount of water resources (Duan et al., 2019). However, compared with the past, the retreat of the Aral Sea has slowed in recent years, so it is very meaningful to analyze the changing trends of the Aral Sea since 1960 and the reasons for such changes.
In recent years, with the development and application of the remote sensing technology, many scholars have used remote sensing images to obtain information on dynamic changes of lakes, and to explore the driving forces from natural and human factors (Hanrahan et al., 2009; Yang and Lu, 2014; Jin et al., 2017; Tan et al., 2017; Jing et al., 2018; Zhang et al., 2018). Based on the water balance method, Lei et al. (2014) investigated the dynamics of inland lakes in the Tibetan Plateau and analyzed the effect of climate change on lake dynamics, proposing that the significant increase of regional precipitation is the main reason for lake growth. Li et al. (2017) analyzed the dynamic of Dalinor Lakes based on the Landsat images, and examined its relationship with climatic factors and vegetation changes by using the Grey Relational analysis. Liu et al. (2019) analyzed the interannual and seasonal changes of the lakes in Central Asia from 2001 to 2016 and the driving forces by using the Least Squares Method, and they found that the alpine lakes are mainly affected by climate change, while plains lakes are affected by climate change and human activities. In addition, ESMD is a new method that used to analyze the oscillation period and the nonlinear change of physical, meteorological and hydrological elements, which is approved to be more accurate than the traditional statistical methods (such as the empirical orthogonal functions (EOF) and the moving overages) (Wang et al., 2010; Qin et al., 2019; Zhou et al., 2019). However, few people have applied it to the studies of lake dynamics.
The shrinking of the lake in Central Asia is caused by climate change and human activities (Micklin, 2010; Chen et al., 2017). Rising temperature will increase the frequency of extreme hydrological events and exacerbate the temporal and spatial distribution of water resources (Hagg et al., 2013; Chen et al., 2016a, Chen et al., 2016b; Zhang et al., 2016a, Zhang et al., 2016; Li et al., 2019). White et al. (2014) found that the projected increases in summer temperatures of up to 5 °C by 2070–2099 in the Amu Darya Basin under a high-emission scenario, would lead to an increase in crop water consumptive demand of between 10.6 and 16%. Ozturk et al. (2017) revealed the future climate conditions of the Central Asia based on regional climate model simulations, they showed that the surface air temperatures will increase between 3 °C and about 7 °C, and the precipitation will decrease in almost parts of the region, this will make the ecosystems and social systems more vulnerable. Meanwhile, human activities have also been the main driving forces of the decline in the Aral Sea, especially the massive withdrawal of water from the transboundary rivers (Micklin, 2007). Chen et al. (2018) found that the main reasons for the water resources crisis in the Aral Sea Basin are the mismatched spatial distribution of land and water resources and excessive human activities.
Current research on the Aral Sea mainly focuses on the crisis of the lake's water resources, but the fact that the shrinking rate has slowed down in recent years is equally noteworthy. Thus, in our study, we comprehensively analyzed the change trends of the Aral Sea by using the ESMD method, and attempted to explain the factors causing the slowdown of the Aral Sea retreat. The findings will provide a decision-making reference for the management and protection of the Aral Sea and the formulation of water resources policies. It is also of great significance to improve the efficiency of water resources utilization and the reform of crop planting structure in the basin. Additionally, this study can provide a scientific reference for the construction of “Silk Road economic belt”, as the Aral Sea Basin serves as the core area of the Silk Road.
Section snippets
Study area
The Aral Sea is located on the border of Kazakhstan and Uzbekistan in Central Asia (Fig. 1). It used to be the world's fourth largest lake but has shrunk over the past few decades to a statistically insignificant size. The water supply for the Aral Sea is mainly dependent on the Amu Darya and Syr Darya rivers, which are the two major tributaries of the Aral Sea Basin (Lioubimtseva and Henebry, 2009; Micklin, 2016).
The total area of the Aral Sea Basin measures approximately 1.76 × 104 km2 and
Temporal and spatial variation trends in the Aral Sea
There are two major divisions in the changes of the Aral Sea: in 1986, the main body of the Aral Sea split into two parts- the Large Aral Sea (the South Aral Sea), and the Small Aral Sea (the North Aral Sea). The water resources of the Small Aral Sea mainly come from the Syr Darya River, and the water resources of the Large Aral Sea mainly come from the Amu Darya River. Then, in 2007, the Large Aral Sea split into two parts- the East Aral Sea and the West Aral Sea. The water surface area of the
Discussion
The subsequent shrinkage of the Aral Sea has attracted the attention of numerous scholars, who have analyzed the changes in the sea from different perspectives, and all concluded that the Aral Sea has shrunk dramatically (Stanev et al., 2004; Shi et al., 2014; Jin et al., 2017). In the present study, not only did we calculate the dramatic retreat of the Aral Sea (water surface area decreased by 6.19 × 104 km2), we further found that since 2005, the shrinking rate of the Aral Sea has slowed down
Conclusions
Based on the ESMD method and the multiple linear regression model, we analyzed the changes of the Aral Sea and surrounding water bodies, and explored the time for the slowdown of the Aral Sea retreat, then we analyzed the driving forces from the upstream runoff, water withdrawal and water delivery to the Aral Sea. The conclusions are as follows:
Water surface area of the Aral Sea decreased from 6.89 × 104 km2 in 1960 to 0.70 × 104 km2 in 2018. During the same period, the water volume of the sea
Declaration of Competing Interest
The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper.
Acknowledgement
This work was supported by the National Natural Science Foundation of China [U1903208,41630859] and the Key Research Program of the Chinese Academy of Sciences [ZDRWZS-2019-3].
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