GSTDTAP  > 地球科学
DOI10.5194/acp-20-3459-2020
Low-level mixed-phase clouds in a complex Arctic environment
Gierens, Rosa1; Kneifel, Stefan1; Shupe, Matthew D.2,3; Ebell, Kerstin1; Maturilli, Marion4; Loehnert, Ulrich1
2020-03-24
发表期刊ATMOSPHERIC CHEMISTRY AND PHYSICS
ISSN1680-7316
EISSN1680-7324
出版年2020
卷号20期号:6页码:3459-3481
文章类型Article
语种英语
国家Germany; USA
英文摘要

Low-level mixed-phase clouds (MPCs) are common in the Arctic. Both local and large-scale phenomena influence the properties and lifetime of MPCs. Arctic fjords are characterized by complex terrain and large variations in surface properties. Yet, not many studies have investigated the impact of local boundary layer dynamics and their relative importance on MPCs in the fjord environment. In this work, we used a combination of ground-based remote sensing instruments, surface meteorological observations, radiosoundings, and reanalysis data to study persistent low-level MPCs at Ny-Alesund, Svalbard, for a 2.5-year period. Methods to identify the cloud regime, surface coupling, and regional and local wind patterns were developed. We found that persistent low-level MPCs were most common with westerly winds, and the westerly clouds had a higher mean liquid (42 g m(-2)) and ice water path (16 g m(-2)) compared to those with easterly winds. The increased height and rarity of persistent MPCs with easterly free-tropospheric winds suggest the island and its orography have an influence on the studied clouds. Seasonal variation in the liquid water path was found to be minimal, although the occurrence of persistent MPCs, their height, and their ice water path all showed notable seasonal dependency. Most of the studied MPCs were decoupled from the surface (63 %-82 % of the time). The coupled clouds had 41 % higher liquid water path than the fully decoupled ones. Local winds in the fjord were related to the frequency of surface coupling, and we propose that katabatic winds from the glaciers in the vicinity of the station may cause clouds to decouple. We concluded that while the regional to large-scale wind direction was important for the persistent MPC occurrence and properties, the local-scale phenomena (local wind patterns in the fjord and surface coupling) also had an influence. Moreover, this suggests that local boundary layer processes should be described in models in order to present low-level MPC properties accurately.


领域地球科学
收录类别SCI-E
WOS记录号WOS:000521948300002
WOS关键词BOUNDARY-LAYER ; NY-ALESUND ; SEA-ICE ; THERMODYNAMIC STRUCTURE ; SURFACE ; STRATOCUMULUS ; TEMPERATURE ; LIQUID ; VARIABILITY ; STATISTICS
WOS类目Environmental Sciences ; Meteorology & Atmospheric Sciences
WOS研究方向Environmental Sciences & Ecology ; Meteorology & Atmospheric Sciences
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文献类型期刊论文
条目标识符http://119.78.100.173/C666/handle/2XK7JSWQ/278704
专题地球科学
作者单位1.Univ Cologne, Inst Geophys & Meteorol, Cologne, Germany;
2.Univ Colorado, Cooperat Inst Res Environm Sci, Boulder, CO 80309 USA;
3.NOAA, Earth Syst Res Lab, Boulder, CO USA;
4.Helmholtz Ctr Polar & Marine Res, Alfred Wegener Inst, Potsdam, Germany
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Gierens, Rosa,Kneifel, Stefan,Shupe, Matthew D.,et al. Low-level mixed-phase clouds in a complex Arctic environment[J]. ATMOSPHERIC CHEMISTRY AND PHYSICS,2020,20(6):3459-3481.
APA Gierens, Rosa,Kneifel, Stefan,Shupe, Matthew D.,Ebell, Kerstin,Maturilli, Marion,&Loehnert, Ulrich.(2020).Low-level mixed-phase clouds in a complex Arctic environment.ATMOSPHERIC CHEMISTRY AND PHYSICS,20(6),3459-3481.
MLA Gierens, Rosa,et al."Low-level mixed-phase clouds in a complex Arctic environment".ATMOSPHERIC CHEMISTRY AND PHYSICS 20.6(2020):3459-3481.
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