CCPortal
DOI10.5194/acp-21-16925-2021
Sources and nature of ice-nucleating particles in the free troposphere at Jungfraujoch in winter 2017
Lacher L.; Clemen H.-C.; Shen X.; Mertes S.; Gysel-Beer M.; Moallemi A.; Steinbacher M.; Henne S.; Saathoff H.; Mohler O.; Hohler K.; Schiebel T.; Weber D.; Schrod J.; Schneider J.; Kanji Z.A.
发表日期2021
ISSN1680-7316
起始页码16925
结束页码16953
卷号21期号:22
英文摘要Primary ice formation in mixed-phase clouds is initiated by a minute subset of the ambient aerosol population, called ice-nucleating particles (INPs). The knowledge about their atmospheric concentration, composition, and source in cloud-relevant environments is still limited. During the 2017 joint INUIT/CLACE (Ice Nuclei research UnIT/CLoud-Aerosol Characterization Experiment) field campaign, observations of INPs as well as of aerosol physical and chemical properties were performed, complemented by source region modeling. This aimed at investigating the nature and sources of INPs. The campaign took place at the High-Altitude Research Station Jungfraujoch (JFJ), a location where mixed-phase clouds frequently occur. Due to its altitude of 3580gmga.s.l., the station is usually located in the lower free troposphere, but it can also receive air masses from terrestrial and marine sources via long-range transport. INP concentrations were quasi-continuously detected with the Horizontal Ice Nucleation Chamber (HINC) under conditions representing the formation of mixed-phase clouds at -31ggC. The INP measurements were performed in parallel to aerosol measurements from two single-particle mass spectrometers, the Aircraft-based Laser ABlation Aerosol MAss Spectrometer (ALABAMA) and the laser ablation aerosol particle time-of-flight mass spectrometer (LAAPTOF). The chemical identity of INPs is inferred by correlating the time series of ion signals measured by the mass spectrometers with the time series of INP measurements. Moreover, our results are complemented by the direct analysis of ice particle residuals (IPRs) by using an ice-selective inlet (Ice-CVI) coupled with the ALABAMA. Mineral dust particles and aged sea spray particles showed the highest correlations with the INP time series. Their role as INPs is further supported by source emission sensitivity analysis using atmospheric transport modeling, which confirmed that air masses were advected from the Sahara and marine environments during times of elevated INP concentrations and ice-active surface site densities. Indeed, the IPR analysis showed that, by number, mineral dust particles dominated the IPR composition (g1/458g%), and biological and metallic particles are also found to a smaller extent (g1/410g% each). Sea spray particles are also found as IPRs (17g%), and their fraction in the IPRs strongly varied according to the increased presence of small IPRs, which is likely due to an impact from secondary ice crystal formation. This study shows the capability of combining INP concentration measurements with chemical characterization of aerosol particles using single-particle mass spectrometry, source region modeling, and analysis of ice residuals in an environment directly relevant for mixed-phase cloud formation. © 2021 Copernicus GmbH. All rights reserved.
语种英语
scopus关键词aerosol formation; atmospheric modeling; concentration (composition); ice; source identification; troposphere; winter; Bern [Switzerland]; Jungfraujoch; Switzerland
来源期刊ATMOSPHERIC CHEMISTRY AND PHYSICS
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/246423
作者单位Department of Environmental System Sciences, Institute for Atmospheric and Climate Science, ETH Zurich, Zurich, 8092, Switzerland; Particle Chemistry Department, Max Planck Institute for Chemistry, Mainz, 55128, Germany; Institute of Meteorology and Climate Research, Karlsruhe Institute of Technology, Eggenstein-Leopoldshafen, 76344, Germany; Leibniz Institute for Tropospheric Research, Leipzig, 04318, Germany; Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, Villigen, 5232, Switzerland; Empa, Swiss Federal Laboratories for Materials Science and Technology, Dubendorf, 8600, Switzerland; Institute for Atmospheric and Environmental Sciences, Goethe University Frankfurt, Frankfurt, 60438, Germany; Department of Earth, Atmospheric, and Planetary Sciences, Purdue University, West Lafayette, IN 47907, United States; Federal Waterways Engineering and Research Institute, Karlsruhe, 76187, Germany
推荐引用方式
GB/T 7714
Lacher L.,Clemen H.-C.,Shen X.,et al. Sources and nature of ice-nucleating particles in the free troposphere at Jungfraujoch in winter 2017[J],2021,21(22).
APA Lacher L..,Clemen H.-C..,Shen X..,Mertes S..,Gysel-Beer M..,...&Kanji Z.A..(2021).Sources and nature of ice-nucleating particles in the free troposphere at Jungfraujoch in winter 2017.ATMOSPHERIC CHEMISTRY AND PHYSICS,21(22).
MLA Lacher L.,et al."Sources and nature of ice-nucleating particles in the free troposphere at Jungfraujoch in winter 2017".ATMOSPHERIC CHEMISTRY AND PHYSICS 21.22(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
[Lacher L.]的文章
[Clemen H.-C.]的文章
[Shen X.]的文章
百度学术
百度学术中相似的文章
[Lacher L.]的文章
[Clemen H.-C.]的文章
[Shen X.]的文章
必应学术
必应学术中相似的文章
[Lacher L.]的文章
[Clemen H.-C.]的文章
[Shen X.]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。