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DOI10.5194/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
ISSN1680-7316
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
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
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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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