共 41 条
Simulation of a Severe Sand and Dust Storm Event in March 2021 in Northern China: Dust Emission Schemes Comparison and the Role of Gusty Wind
被引:6
作者:

Wang, Jikang
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China Meteorol Adm, Natl Meteorol Ctr, Beijing 100081, Peoples R China China Meteorol Adm, Natl Meteorol Ctr, Beijing 100081, Peoples R China

Zhang, Bihui
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China Meteorol Adm, Natl Meteorol Ctr, Beijing 100081, Peoples R China China Meteorol Adm, Natl Meteorol Ctr, Beijing 100081, Peoples R China

Zhang, Hengde
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机构:
China Meteorol Adm, Natl Meteorol Ctr, Beijing 100081, Peoples R China China Meteorol Adm, Natl Meteorol Ctr, Beijing 100081, Peoples R China

Hua, Cong
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China Meteorol Adm, Natl Meteorol Ctr, Beijing 100081, Peoples R China China Meteorol Adm, Natl Meteorol Ctr, Beijing 100081, Peoples R China

An, Linchang
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China Meteorol Adm, Natl Meteorol Ctr, Beijing 100081, Peoples R China China Meteorol Adm, Natl Meteorol Ctr, Beijing 100081, Peoples R China

Gui, Hailin
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h-index: 0
机构:
China Meteorol Adm, Natl Meteorol Ctr, Beijing 100081, Peoples R China China Meteorol Adm, Natl Meteorol Ctr, Beijing 100081, Peoples R China
机构:
[1] China Meteorol Adm, Natl Meteorol Ctr, Beijing 100081, Peoples R China
来源:
基金:
中国国家自然科学基金;
关键词:
sand and dust storms;
gusty-wind model;
vertical dust flux parameterizations;
CAMx;
COHERENT STRUCTURE;
EAST-ASIA;
MODEL;
CLIMATE;
PARAMETERIZATION;
PREDICTION;
GUSTINESS;
IMPACT;
SPEED;
PM10;
D O I:
10.3390/atmos13010108
中图分类号:
X [环境科学、安全科学];
学科分类号:
08 ;
0830 ;
摘要:
Northern China experienced a severe sand and dust storm (SDS) on 14/15 March 2021. It was difficult to simulate this severe SDS event accurately. This study compared the performances of three dust-emission schemes on simulating PM10 concentration during this SDS event by implementing three vertical dust flux parameterizations in the Comprehensive Air-Quality Model with Extensions (CAMx) model. Additionally, a statistical gusty-wind model was implemented in the dust-emission scheme, and it was used to quantify the gusty-wind contribution to dust emissions and peak PM10 concentration. As a result, the LS scheme (Lu and Shao 1999) produced the minimum errors for peak PM10 concentrations, the MB scheme (Marticorena and Bergametti 1995) underestimated the PM10 concentrations by 70-90%, and the KOK scheme (Kok et al. 2014) overestimated PM10 concentrations by 10-50% in most areas. The gusty-wind model could reasonably reproduce the probability density function of 2-min wind speeds. There were 5-40% more dust-emission flux and 5-40% more peak PM10 concentrations generated by the gusty wind than the hourly wind in the dust-source regions. The increase of peak PM10 concentration caused by gusty wind in the non-dust-source regions was higher than in the dust-source regions, with 10-50%. Implementing the gusty-wind model could help improve the LS scheme's performance in simulating PM10 concentrations of this severe SDS event. More work is still needed to investigate the reliability of the gusty-wind model and LS scheme on various SDS events.
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