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DOI | 10.5194/acp-20-29-2020 |
Modelling the relationship between liquid water content and cloud droplet number concentration observed in low clouds in the summer Arctic and its radiative effects | |
Dionne J.; Von Salzen K.; Cole J.; Mahmood R.; Richard Leaitch W.; Lesins G.; Folkins I.; Chang R.Y.-W. | |
发表日期 | 2020 |
ISSN | 1680-7316 |
起始页码 | 29 |
结束页码 | 43 |
卷号 | 20期号:1 |
英文摘要 | Low clouds persist in the summer Arctic with important consequences for the radiation budget. In this study, we simulate the linear relationship between liquid water content (LWC) and cloud droplet number concentration (CDNC) observed during an aircraft campaign based out of Resolute Bay, Canada, conducted as part of the Network on Climate and Aerosols: Addressing Key Uncertainties in Remote Canadian Environments study in July 2014. Using a singlecolumn model, we find that autoconversion can explain the observed linear relationship between LWC and CDNC. Of the three autoconversion schemes we examined, the scheme using continuous drizzle (Khairoutdinov and Kogan, 2000) appears to best reproduce the observed linearity in the tenuous cloud regime (Mauritsen et al., 2011), while a scheme with a threshold for rain (Liu and Daum, 2004) best reproduces the linearity at higher CDNC. An offline version of the radiative transfer model used in the Canadian Atmospheric Model version 4.3 is used to compare the radiative effects of the modelled and observed clouds. We find that there is no significant difference in the upward longwave cloud radiative effect at the top of the atmosphere from the three autoconversion schemes (p = 0.05) but that all three schemes differ at p = 0.05 from the calculations based on observations. In contrast, the downward longwave and shortwave cloud radiative effect at the surface for the Wood (2005b) and Khairoutdinov and Kogan (2000) schemes do not differ significantly (p = 0.05) from the observation-based radiative calculations, while the Liu and Daum (2004) scheme differs significantly from the observation-based calculation for the downward shortwave but not the downward longwave fluxes. © Author(s) 2020. |
语种 | 英语 |
scopus关键词 | atmospheric modeling; cloud droplet; concentration (composition); radiation budget; radiative transfer; summer; water content; Arctic; Canada; Cornwallis Island; Nunavut; Queen Elizabeth Islands; Resolute Bay |
来源期刊 | Atmospheric Chemistry and Physics
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文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/141637 |
作者单位 | Physics and Atmospheric Science Department, Dalhousie University, Halifax, NS, Canada; Climate Research Division, Science and Technology Branch, Environment and Climate Change Canada, Toronto, ON, Canada; School of Earth and Ocean Sciences, University of VictoriaVIC, Canada; Earth, Ocean, and Atmospheric Sciences Department, University of British Columbia, Vancouver, BC, Canada; Barcelona Supercomputing Center, Barcelona, Spain |
推荐引用方式 GB/T 7714 | Dionne J.,Von Salzen K.,Cole J.,et al. Modelling the relationship between liquid water content and cloud droplet number concentration observed in low clouds in the summer Arctic and its radiative effects[J],2020,20(1). |
APA | Dionne J..,Von Salzen K..,Cole J..,Mahmood R..,Richard Leaitch W..,...&Chang R.Y.-W..(2020).Modelling the relationship between liquid water content and cloud droplet number concentration observed in low clouds in the summer Arctic and its radiative effects.Atmospheric Chemistry and Physics,20(1). |
MLA | Dionne J.,et al."Modelling the relationship between liquid water content and cloud droplet number concentration observed in low clouds in the summer Arctic and its radiative effects".Atmospheric Chemistry and Physics 20.1(2020). |
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