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Meteorological conditions during the ACLOUD/PASCAL field campaign near Svalbard in early summer 2017

  • The two concerted field campaigns, Arctic CLoud Observations Using airborne measurements during polar Day (ACLOUD) and the Physical feedbacks of Arctic planetary boundary level Sea ice, Cloud and AerosoL (PASCAL), took place near Svalbard from 23 May to 26 June 2017. They were focused on studying Arctic mixed-phase clouds and involved observations from two airplanes (ACLOUD), an icebreaker (PASCAL) and a tethered balloon, as well as ground-based stations. Here, we present the synoptic development during the 35-day period of the campaigns, using near-surface and upper-air meteorological observations, as well as operational satellite, analysis, and reanalysis data. Over the campaign period, short-term synoptic variability was substantial, dominating over the seasonal cycle. During the first campaign week, cold and dry Arctic air from the north persisted, with a distinct but seasonally unusual cold air outbreak. Cloudy conditions with mostly low-level clouds prevailed. The subsequent 2 weeks were characterized by warm and moist maritimeThe two concerted field campaigns, Arctic CLoud Observations Using airborne measurements during polar Day (ACLOUD) and the Physical feedbacks of Arctic planetary boundary level Sea ice, Cloud and AerosoL (PASCAL), took place near Svalbard from 23 May to 26 June 2017. They were focused on studying Arctic mixed-phase clouds and involved observations from two airplanes (ACLOUD), an icebreaker (PASCAL) and a tethered balloon, as well as ground-based stations. Here, we present the synoptic development during the 35-day period of the campaigns, using near-surface and upper-air meteorological observations, as well as operational satellite, analysis, and reanalysis data. Over the campaign period, short-term synoptic variability was substantial, dominating over the seasonal cycle. During the first campaign week, cold and dry Arctic air from the north persisted, with a distinct but seasonally unusual cold air outbreak. Cloudy conditions with mostly low-level clouds prevailed. The subsequent 2 weeks were characterized by warm and moist maritime air from the south and east, which included two events of warm air advection. These synoptical disturbances caused lower cloud cover fractions and higher-reaching cloud systems. In the final 2 weeks, adiabatically warmed air from the west dominated, with cloud properties strongly varying within the range of the two other periods. Results presented here provide synoptic information needed to analyze and interpret data of upcoming studies from ACLOUD/PASCAL, while also offering unprecedented measurements in a sparsely observed region.show moreshow less

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Author details:Erlend Moster KnudsenORCiD, Bernd HeinoldGND, Sandro DahlkeORCiD, Heiko BozemORCiDGND, Susanne CrewellORCiDGND, Irina V. GorodetskayaORCiD, Georg HeygsterORCiD, Daniel KunkelORCiDGND, Marion MaturilliORCiD, Mario MechORCiDGND, Carolina VicetoORCiD, Annette RinkeORCiDGND, Holger SchmithusenORCiD, Andre EhrlichORCiDGND, Andreas MackeORCiDGND, Christof LüpkesORCiD, Manfred WendischORCiDGND
DOI:https://doi.org/10.5194/acp-18-17995-2018
ISSN:1680-7316
ISSN:1680-7324
Title of parent work (English):Atmospheric chemistry and physics
Publisher:Copernicus
Place of publishing:Göttingen
Publication type:Article
Language:English
Year of first publication:2018
Publication year:2018
Release date:2020/05/13
Volume:18
Issue:24
Number of pages:28
First page:17995
Last Page:18022
Funding institution:German Research Foundation (DFG)
Funding number:TRR 172 268020496
Organizational units:Mathematisch-Naturwissenschaftliche Fakultät / Institut für Geowissenschaften
Peer review:Referiert
Publishing method:Open Access
Open Access / Gold Open-Access
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