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DOI | 10.1175/JCLI-D-19-0481.1 |
Spring Dust Mass Flux over the Tibetan Plateau during 2007-19 and Connections with North Atlantic SST Variability | |
Xu, Chao; Ma, Yaoming; Ma, Jiehua; You, Chao; Wang, Huijun | |
通讯作者 | Xu, C (通讯作者) |
发表日期 | 2020 |
ISSN | 0894-8755 |
EISSN | 1520-0442 |
起始页码 | 9691 |
结束页码 | 9703 |
卷号 | 33期号:22 |
英文摘要 | Dust is the major aerosol type over the Tibetan Plateau (TP), and the TP plays an important role in forming the spring dust belt across the Northern Hemisphere in the upper troposphere. Estimated spring dust mass flux (DMF) showed a significant declining trend over the TP during 2007-19. The total spring DMF across the TP (TDMFTP) was mainly affected by DMFs over the Tarim Basin, while the spring DMF across the TP in the midtroposphere was also connected with DMFs over the northwest Indian Peninsula and central Asia. Interannual variability of springTDMFTP was strongly correlated with the North Atlantic winter sea surface temperature (SST) tripole. A cold preceding winter induced by the North Atlantic winter SST tripole over midlatitude Eurasia promotes dust activities in the subsequent spring. The North Atlantic winter SST tripole anomalies persist into the subsequent spring and induce a corresponding atmosphere response. Enhanced atmospheric baroclinicity develops over northwest China and the northern Indian Peninsula during spring, which is attributed to surface thermal forcing induced by the positive winter SST tripole phase. A strong positive North Atlantic winter SST tripole anomaly strengthens the upper-level westerly jets, enhancing airflow toward the TP midtroposphere; together, these circulation patterns cause anomalous cyclonic conditions in the lower troposphere, especially over the Tarim Basin, via the eastward propagation of a Rossby wave train. These atmospheric circulation conditions are likely to increase the frequency of dust occurrence and promote the transport of dust onto the TP. |
关键词 | OPTICAL DEPTH RETRIEVALSAEROSOL CLASSIFICATIONWEATHER FREQUENCYCYCLONE ACTIVITYOSCILLATION NAOLIDAR RATIOSUMMERTRANSPORTREANALYSISIMPACTS |
英文关键词 | Dust or dust storms; Sea surface temperature; Interannual variability; Spring season; Aerosol optical properties |
语种 | 英语 |
WOS研究方向 | Meteorology & Atmospheric Sciences |
WOS类目 | Meteorology & Atmospheric Sciences |
WOS记录号 | WOS:000589812200012 |
来源期刊 | JOURNAL OF CLIMATE |
来源机构 | 中国科学院青藏高原研究所 |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/259868 |
推荐引用方式 GB/T 7714 | Xu, Chao,Ma, Yaoming,Ma, Jiehua,et al. Spring Dust Mass Flux over the Tibetan Plateau during 2007-19 and Connections with North Atlantic SST Variability[J]. 中国科学院青藏高原研究所,2020,33(22). |
APA | Xu, Chao,Ma, Yaoming,Ma, Jiehua,You, Chao,&Wang, Huijun.(2020).Spring Dust Mass Flux over the Tibetan Plateau during 2007-19 and Connections with North Atlantic SST Variability.JOURNAL OF CLIMATE,33(22). |
MLA | Xu, Chao,et al."Spring Dust Mass Flux over the Tibetan Plateau during 2007-19 and Connections with North Atlantic SST Variability".JOURNAL OF CLIMATE 33.22(2020). |
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