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Title: Simulated precipitation changes in Central Asia since the Last Glacial Maximum

Journal Article · · Quaternary International
 [1];  [1];  [1];  [2]
  1. Lanzhou Univ. (China). MOE Key Lab. of Western China's Environmental System, College of Earth and Environmental Sciences
  2. Chengdu University of Information Technology, Chengdu (China). School of Atmospheric Sciences; Lanzhou Univ. (China). MOE Key Lab. of Western China's Environmental System, College of Earth and Environmental Sciences

According to the article, the availability of freshwater has been and remains a crucial concern in westerlies-dominated arid Central Asia. Understanding precipitation changes in this area and the underlying mechanisms, therefore, is of great importance. This study explores precipitation changes in Central Asia (35°–50° N and 50°–70° E) since the Last Glacial Maximum (LGM) and their control factors using results from the “Simulation of Transient Climate Evolution over the last 21,000 years”. Transient simulations reveal that a wet climate occurred during the LGM, the Bølling-Allerød warm period, and the middle Holocene, and a dry climate occurred during Heinrich event 1, the Younger Dryas, and the early Holocene in this area. Model results are in good agreement with proxy records since the last deglaciation. These changes were mainly controlled by Earth's orbital parameters, meltwater discharges into the oceans and continental ice sheets. The contribution of GHG concentrations to precipitation changes was minor. External forcing factors influenced the precipitation mainly through affecting the water vapor input from the North Atlantic and Mediterranean Sea, and vertical motions of the atmosphere over Central Asia. The North Atlantic Oscillation was an important atmospheric bridge connecting the external forcings to precipitation changes in Central Asia. There were complex relationships between precipitation changes in Central Asia and East Asia since the LGM due to the differences of the dominating factors.

Research Organization:
Oak Ridge National Lab. (ORNL), Oak Ridge, TN (United States). Oak Ridge Leadership Computing Facility (OLCF)
Sponsoring Organization:
USDOE Office of Science (SC)
OSTI ID:
1565737
Journal Information:
Quaternary International, Vol. 490, Issue C; ISSN 1040-6182
Publisher:
Elsevier
Country of Publication:
United States
Language:
English

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