CCPortal
DOI10.1029/2020JD033864
Ice-Nucleating Particle Concentrations and Sources in Rainwater Over the Third Pole, Tibetan Plateau
Chen, J.; Wu, Z. J.; Wu, G. M.; Gong, X. D.; Wang, F.; Chen, J. C.; Shi, G. L.; Hu, M.; Cong, Z. Y.
通讯作者Wu, ZJ (通讯作者)
发表日期2021
ISSN2169-897X
EISSN2169-8996
卷号126期号:9
英文摘要The ice-nucleating particles (INPs) modulate the microphysics and radiative properties of clouds. However, less is known concerning their abundance and sources in the most pristine and climatic sensitive regions, such as the Tibetan Plateau (TP). Here, to our best knowledge, we conduct the first investigation on INPs in rainwater collected in the TP region under mixed-phase cloud conditions. The value of INP concentrations varies from 0.002 to 0.675 L-1 air over the temperature range from -7.1 to -27.5 degrees C. This is within the INP spectra derived from precipitation under worldwide geophysical conditions and is also comparable with INP concentrations in the Arctic regions. The heat-sensitive INPs account for 57% +/- 30% of the observed INPs at -20 degrees C and become increasingly important at higher temperatures, indicating biological particles as major contributors to INPs at temperatures above -20 degrees C over the TP, especially on the day with additional input of biogenic materials carried by dust particles. Chemical analysis demonstrates that the rainwater components are mixture of dust particles, marine aerosol, and anthropogenic pollutants. Combined with the backward trajectory analysis, we show that dust particles transported from the surrounding deserts and originated from ground surface of TP may contribute to the heat-resistant INPs at temperatures below -20 degrees C. Plain Language Summary Ice-nucleating particles (INPs) can catalyze the ice crystal formation through heterogeneous ice nucleation and thus play a profound role in the aerosol-cloud interaction. The Tibetan Plateau (TP) is one of the most vulnerable climate systems in the word, but we have very less knowledge on INPs over the TP, impeding our understanding of the aerosol-cloud interaction in this region. Here, the INP number concentrations and sources are quantified and identified over the TP under conditions relevant to mixed-phase clouds on a basis of comprehensive study on chemical composition and INP properties of rainwater. We show that biological particles are the dominant contributor of INPs at temperatures above -20 degrees C. The rainwater chemical components are mixtures of dust, marine aerosol, and anthropogenic pollutants. Dust particles may contribute to the heat-resistant INPs at temperatures below -20 degrees C.
关键词IMMERSION FREEZING BEHAVIORSOURCE APPORTIONMENTAIR-POLLUTIONBLACK CARBONMICROPHYSICAL PROPERTIESPARTICULATE-MATTERASH PARTICLESNAM COPRECIPITATIONAEROSOL
语种英语
WOS研究方向Meteorology & Atmospheric Sciences
WOS类目Meteorology & Atmospheric Sciences
WOS记录号WOS:000656152800023
来源期刊JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES
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/260501
推荐引用方式
GB/T 7714
Chen, J.,Wu, Z. J.,Wu, G. M.,et al. Ice-Nucleating Particle Concentrations and Sources in Rainwater Over the Third Pole, Tibetan Plateau[J]. 中国科学院青藏高原研究所,2021,126(9).
APA Chen, J..,Wu, Z. J..,Wu, G. M..,Gong, X. D..,Wang, F..,...&Cong, Z. Y..(2021).Ice-Nucleating Particle Concentrations and Sources in Rainwater Over the Third Pole, Tibetan Plateau.JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES,126(9).
MLA Chen, J.,et al."Ice-Nucleating Particle Concentrations and Sources in Rainwater Over the Third Pole, Tibetan Plateau".JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES 126.9(2021).
条目包含的文件
条目无相关文件。
个性服务
推荐该条目
保存到收藏夹
导出为Endnote文件
谷歌学术
谷歌学术中相似的文章
[Chen, J.]的文章
[Wu, Z. J.]的文章
[Wu, G. M.]的文章
百度学术
百度学术中相似的文章
[Chen, J.]的文章
[Wu, Z. J.]的文章
[Wu, G. M.]的文章
必应学术
必应学术中相似的文章
[Chen, J.]的文章
[Wu, Z. J.]的文章
[Wu, G. M.]的文章
相关权益政策
暂无数据
收藏/分享

除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。