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DOI10.5194/acp-22-9767-2022
Retrieving ice-nucleating particle concentration and ice multiplication factors using active remote sensing validated by in situ observations
Wieder, Joerg; Ihn, Nikola; Mignani, Claudia; Haarig, Moritz; Buehl, Johannes; Seifert, Patric; Engelmann, Ronny; Ramelli, Fabiola; Kanji, Zamin A.; Lohmann, Ulrike; Henneberger, Jan
发表日期2022
ISSN1680-7316
EISSN1680-7324
起始页码9767
结束页码9797
卷号22期号:15页码:31
英文摘要Understanding the evolution of the ice phase within mixed-phase clouds (MPCs) is necessary to reduce uncertainties related to the cloud radiative feedback in climate projections and precipitation initiation. Both primary ice formation via ice-nucleating particles (INPs) and secondary ice production (SIP) within MPCs are unconstrained, not least because of the lack of atmospheric observations. In the past decades, advanced remote sensing methods have emerged which provide high-resolution data of aerosol and cloud properties and could be key in understanding microphysical processes on a global scale. In this study, we retrieved INP concentrations and ice multiplication factors (IMFs) in wintertime orographic clouds using active remote sensing and in situ observations obtained during the RACLETS campaign in the Swiss Alps. INP concentrations in air masses dominated by Saharan dust and continental aerosol were retrieved from a polarization Raman lidar and validated with aerosol and INP in situ observations on a mountaintop. A calibration factor of 0.0204 for the global INP parameterization by is derived by comparing in situ aerosol and INP measurements, improving the INP concentration retrieval for continental aerosols. Based on combined lidar and radar measurements, the ice crystal number concentration and ice water content were retrieved and validated with balloon-borne in situ observations, which agreed with the balloon-borne in situ observations within an order of magnitude. For seven cloud cases the ice multiplication factors (IMFs), defined as the quotient of the ice crystal number concentration to the INP concentration, were calculated. The median IMF was around 80, and SIP was active (defined as IMFs > 1) nearly 85 % of the time. SIP was found to be active at all observed temperatures (-30 to -5 degrees C), with the highest IMFs between -20 and -5 degrees C. The introduced methodology could be extended to larger datasets to better understand the impact of SIP not only over the Alps but also at other locations and for other cloud types.
学科领域Environmental Sciences; Meteorology & Atmospheric Sciences
语种英语
WOS研究方向Environmental Sciences & Ecology ; Meteorology & Atmospheric Sciences
WOS记录号WOS:000835525000001
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/273551
作者单位Swiss Federal Institutes of Technology Domain; ETH Zurich; University of Basel; Leibniz Institut fur Tropospharenforschung (TROPOS); Colorado State University
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Wieder, Joerg,Ihn, Nikola,Mignani, Claudia,et al. Retrieving ice-nucleating particle concentration and ice multiplication factors using active remote sensing validated by in situ observations[J],2022,22(15):31.
APA Wieder, Joerg.,Ihn, Nikola.,Mignani, Claudia.,Haarig, Moritz.,Buehl, Johannes.,...&Henneberger, Jan.(2022).Retrieving ice-nucleating particle concentration and ice multiplication factors using active remote sensing validated by in situ observations.ATMOSPHERIC CHEMISTRY AND PHYSICS,22(15),31.
MLA Wieder, Joerg,et al."Retrieving ice-nucleating particle concentration and ice multiplication factors using active remote sensing validated by in situ observations".ATMOSPHERIC CHEMISTRY AND PHYSICS 22.15(2022):31.
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