Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.1029/2019JD030753 |
Detection of New Dust Sources in Central/East Asia and Their Impact on Simulations of a Severe Sand and Dust Storm | |
Zhou, Chunhong; Gui, Hailin; Hu, Jiangkai; Ke, Huabing; Wang, Yaqiang; Zhang, Xiaoye | |
通讯作者 | Zhou, CH (corresponding author), Chinese Acad Meteorol Sci, State Key Lab Severe Weather, Beijing, Peoples R China. ; Zhou, CH (corresponding author), Chinese Acad Meteorol Sci, Key Lab Atmospher Chem CMA, Beijing, Peoples R China. ; Hu, JK (corresponding author), Natl Meteorol Ctr, Beijing, Peoples R China. |
来源期刊 | JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES
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ISSN | 2169-897X |
EISSN | 2169-8996 |
出版年 | 2019 |
卷号 | 124期号:17-18页码:10232-10247 |
英文摘要 | Information regarding dust concentrations and size distributions is very important for determining air quality and aerosol-radiation-cloud interactions. Only by using a correct erosion database can the sectional dust emission scheme resolve detailed size distributions and determine where and how dust will be emitted. In this paper, the bias and reasons for dust emission in China Meteorological Administration Unified Atmospheric Chemistry Environment-Dust, an operational dust forecasting model, are analyzed using a heavy sand and dust storm episode. We used 18 years of routine sand and dust storm phenomena recorded at meteorological stations to retrieve and update the desertification details in the MBA sectional dust emission scheme adopted in China Meteorological Administration Unified Atmospheric Chemistry Environment-Dust. New desertification details include decreased erodibility in the area adjacent to Uzbekistan, Turkmenistan, and southern Kazakhstan, where Kyzylkum, Karakum, and Aralkum are located in central Asia, and in the Chinese deserts of Onqin Daga, Mu Us, and Gurbantungut. New desertification also results in increased erodibility in northern Mongolia. Comparisons show that the new desertification database decreases overestimation of dust emission in central Asia, including western Mongolia. It improves the underestimation of dust emission in northern Mongolia and the Gobi desert in southeast Mongolia, and the Taklimakan desert in China. Consequently, it corrects the overestimated dust cloud in the source area and in areas impacted by dust transportation. The timing, quantitative mass concentrations, and dust size distributions determined here are all more reasonable and rational than those of the original case. |
类型 | Article |
语种 | 英语 |
开放获取类型 | hybrid |
收录类别 | SCI-E |
WOS记录号 | WOS:000494747300026 |
WOS关键词 | MINERAL AEROSOL PRODUCTION ; WIND EROSION ; SIZE DISTRIBUTIONS ; SOIL-MOISTURE ; TRANSPORT ; EMISSION ; DESERT ; THRESHOLD ; MODEL ; ENTRAINMENT |
WOS类目 | Meteorology & Atmospheric Sciences |
WOS研究方向 | Meteorology & Atmospheric Sciences |
资源类型 | 期刊论文 |
条目标识符 | http://119.78.100.177/qdio/handle/2XILL650/369712 |
作者单位 | [Zhou, Chunhong; Ke, Huabing; Wang, Yaqiang; Zhang, Xiaoye] Chinese Acad Meteorol Sci, State Key Lab Severe Weather, Beijing, Peoples R China; [Zhou, Chunhong; Ke, Huabing; Wang, Yaqiang; Zhang, Xiaoye] Chinese Acad Meteorol Sci, Key Lab Atmospher Chem CMA, Beijing, Peoples R China; [Gui, Hailin; Hu, Jiangkai] Natl Meteorol Ctr, Beijing, Peoples R China; [Zhang, Xiaoye] Chinese Acad Sci, IUE, Ctr Excellence Reg Atmospher Environm, Xiamen, Fujian, Peoples R China |
推荐引用方式 GB/T 7714 | Zhou, Chunhong,Gui, Hailin,Hu, Jiangkai,et al. Detection of New Dust Sources in Central/East Asia and Their Impact on Simulations of a Severe Sand and Dust Storm[J],2019,124(17-18):10232-10247. |
APA | Zhou, Chunhong,Gui, Hailin,Hu, Jiangkai,Ke, Huabing,Wang, Yaqiang,&Zhang, Xiaoye.(2019).Detection of New Dust Sources in Central/East Asia and Their Impact on Simulations of a Severe Sand and Dust Storm.JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES,124(17-18),10232-10247. |
MLA | Zhou, Chunhong,et al."Detection of New Dust Sources in Central/East Asia and Their Impact on Simulations of a Severe Sand and Dust Storm".JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES 124.17-18(2019):10232-10247. |
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