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DOI | 10.5194/acp-21-4149-2021 |
Processes contributing to cloud dissipation and formation events on the North Slope of Alaska | |
Sedlar J.; Igel A.; Telg H. | |
发表日期 | 2021 |
ISSN | 1680-7316 |
起始页码 | 4149 |
结束页码 | 4167 |
卷号 | 21期号:5 |
英文摘要 | Clear-sky periods across the high latitudes have profound impacts on the surface energy budget and lower atmospheric stratification; however an understanding of the atmospheric processes leading to low-level cloud dissipation and formation events is limited. A method to identify clear periods at UtqiaÄ¡vik (formerly Barrow), Alaska, during a 5-year period (2014-2018) is developed. A suite of remote sensing and in situ measurements from the high-latitude observatory are analyzed; we focus on comparing and contrasting atmospheric properties during low-level (below 2 km) cloud dissipation and formation events to understand the processes controlling clear-sky periods. Vertical profiles of lidar backscatter suggest that aerosol presence across the lower atmosphere is relatively invariant during the periods bookending clear conditions, which suggests that a sparsity of aerosol is not frequently a cause for cloud dissipation on the North Slope of Alaska. Further, meteorological analysis indicates two active processes ongoing that appear to support the formation of low clouds after a clear-sky period: namely, horizontal advection, which was dominant in winter and early spring, and quiescent air mass modification, which was dominant in the summer. During summer, the dominant mode of cloud formation is a low cloud or fog layer developing near the surface. This low cloud formation is driven largely by air mass modification under relatively quiescent synoptic conditions. Near-surface aerosol particles concentrations changed by a factor of 2 around summer formation events. Thermodynamic adjustment and increased aerosol presence under quiescent atmospheric conditions are hypothesized as important mechanisms for fog formation. © Author(s) 2021. This work is distributed under the Creative Commons Attribution 4.0 License. |
语种 | 英语 |
scopus关键词 | advection; aerosol; air mass; backscatter; clear sky; cloud cover; cloud microphysics; energy budget; formation mechanism; in situ measurement; remote sensing; stratification; vertical profile; Alaska; North Slope; United States |
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/247052 |
作者单位 | Cooperative Institute for Research in Environmental Sciences, University of Colorado Boulder, Boulder, CO, United States; Noaa Global Monitoring Laboratory, Boulder, CO, United States; Department of Land Air, and Water Resources, University of California Davis, Davis, CA, United States |
推荐引用方式 GB/T 7714 | Sedlar J.,Igel A.,Telg H.. Processes contributing to cloud dissipation and formation events on the North Slope of Alaska[J],2021,21(5). |
APA | Sedlar J.,Igel A.,&Telg H..(2021).Processes contributing to cloud dissipation and formation events on the North Slope of Alaska.ATMOSPHERIC CHEMISTRY AND PHYSICS,21(5). |
MLA | Sedlar J.,et al."Processes contributing to cloud dissipation and formation events on the North Slope of Alaska".ATMOSPHERIC CHEMISTRY AND PHYSICS 21.5(2021). |
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