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Reliable information on the dynamics of hydrological changes is crucial for the social and economic stabilities and sustaining developments in arid Central Asia. However, the few long‐term hydrological records limit understanding of the relationship between meltwater runoff and climate changes, because the short‐term observations show a paradoxical runoff trend with climate warming across Central Asia. Here, we made a systematic analysis on the 10Be exposure ages of the river terraces developed in the eastern Tarim Basin and reconstructed the hydrological regime changes during the past 170 ka. These data, together with the ages of the river terraces in the water source areas, suggest that the exposure ages of river terraces in the eastern Tarim Basin reflect the depositional time of alluvial sediments. The meltwater runoff displays an inverse relation with the North Hemisphere Summer Insolation and temperature changes on both orbital and millennial time scale, indicating that low temperatures favor high runoff fluxes. The observed correlation between the hydrological regimes and temperature changes suggests that the runoff will decrease and thus climate will become drying with global warming in arid Central Asia. Plain Language Summary: Reliable information on the dynamics of hydrological changes is crucial for the social and economic stabilities and sustaining developments in arid Central Asia. However, the short‐term observations show a paradoxical runoff trend with climate warming across Central Asia. In order to understand the association of hydrological regimes with climate changes in arid Central Asia, particularly the hydrological changes on the context of global warming, this study reconstructs the hydrological changes in the eastern Tarim Basin over the past 170 ka. Our results show that the high runoff occurred during low temperature periods in the past. The inverse correlation between the hydrological regimes and temperatures in this study indicates that the runoff will decrease and climate will become drying with global warming in the future. More conservative water management policies should be taken for the sustaining development and water security in Central Asia. Key Points: 10Be exposure ages of river terraces in the eastern Tarim Basin reflect the depositional dates of alluvial sedimentsThe runoff in central Asia displays an inverse relation with global temperature changesHigh runoffs and humid climates occurred during cold periods over the past 170 ka, indicating a climate drying with global warming [ABSTRACT FROM AUTHOR]

Both wind strength and anthropogenic emissions have been assumed to be the dominant factors in determining the occurrence of hazy weather in China. However, few records are available with sufficient temporal length and resolution, which enable the two signals to be separated, and hence address the dynamics of haze days and the global impact of the anthropogenic emissions in China, particularly in the context of global warming. Here we present the first long‐term (last ~180 years) lake sediment records of changes in wind strength and atmospheric loading of anthropogenic emissions in China. Our results show that the atmospheric loading of anthropogenic emissions and haze formation are closely related to the changes in wind strength associated with temperature changes, which are likely forced by tropical sea surface temperature. Comparison of our results with Pb isotope records from Japan and with the record of Pb concentrations in Greenland ice core indicates that the anthropogenic pollutants emitted in China stagnate mainly over the source area and neighboring regions, which thus favors haze formation under a warming climate. However, they would be transported worldwide under conditions of strong winds and decreased temperature. Climatic warming, together with the periodic changes in temperature, has caused unprecedented heavy haze days in recent decades in China. The observed pattern of periodic temperature variations suggests that in the next ~30 years, wind strength will increase and thus reduce the incidence of haze days. However, this reduction may be attenuated by continued climatic warming as anthropogenic greenhouse gases emissions continue. Key Points: Atmospheric pollutant concentrations decoupled from anthropogenic emissions in ChinaAtmospheric loading of anthropogenic pollutants in China increased with temperature forced by tropical sea surface temperatureAsian anthropogenic pollutants can be transported worldwide under the condition of cold temperature [ABSTRACT FROM AUTHOR]