Weakening Dust Storm Intensity in Arid Central Asia Due to Global Warming Over the Past 160 Years

Dust storms occur frequently in arid central Asia (ACA) and greatly influence the regional ecology/environment, human health, and security, as well as the global climate. To date, neither the patterns nor the underlying mechanisms of dust storms in ACA are fully understood, partly due to the lack of...

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Bibliographic Details
Published in:Frontiers in Earth Science
Main Authors: Zhang, Jin, Xu, Hai, Lan, Jianghu, Ai, Li, Sheng, Enguo, Yan, Dongna, Zhou, Kang'en, Yu, Keke, Song, Yunping, Zhang, Shuang, Torfstein, Adi
Format: Report
Language:English
Published: FRONTIERS MEDIA SA 2020
Subjects:
dust storm
global warming
arid central Asia
Lake Karakul
grain size
MALAN ICE CORE
TIBETAN PLATEAU
ATMOSPHERIC CIRCULATION
EVENT FREQUENCY
SOURCE AREA
RECORD
CHINA
HOLOCENE
DEPOSITS
LAKE
Geology
Geosciences
Multidisciplinary
ice core
Online Access:http://ir.ieecas.cn/handle/361006/15148
https://doi.org/10.3389/feart.2020.00284
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Summary:Dust storms occur frequently in arid central Asia (ACA) and greatly influence the regional ecology/environment, human health, and security, as well as the global climate. To date, neither the patterns nor the underlying mechanisms of dust storms in ACA are fully understood, partly due to the lack of long-term historical records. Here, we reconstruct a dust storm history of the past similar to 160 years in northwest China, based on high-resolution sedimentary proxies retrieved from Lake Karakul (located in the core zone of ACA). We find that changes in the sedimentary coarse fraction (grain size > 64 mu m) in Lake Karakul are correlated with both historical and modern observed dust storms. The reconstructed dust storm intensity shows a decreasing trend sinceAD1850s, with three high occurrence intervals atAD1870s-1910s,AD1930s-1940s, andAD1960s-1980s. We contend that changes in temperature and wind speed could have dominated the frequency and intensity of dust storms in northwest China during the record periods: temperature controls the wind speed and then the dust storm frequency/intensity; lower temperature corresponding to higher wind speed, and higher dust storm frequency/intensity, and vice versa. The observed anthropogenic global warming could have led to a decrease in atmospheric temperature gradients and decline in wind speed and then decreasing dust storm frequency/intensity. Providing this stands, less and weaker dust storms are expected under a continuously anthropogenic warming scenario.

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