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

dc.bibliographicCitation.firstPage17995
dc.bibliographicCitation.issue24
dc.bibliographicCitation.lastPage18022
dc.bibliographicCitation.volume18
dc.contributor.authorKnudsen, Erlend M.
dc.contributor.authorHeinold, Bernd
dc.contributor.authorDahlke, Sandro
dc.contributor.authorBozem, Heiko
dc.contributor.authorCrewell, Susanne
dc.contributor.authorGorodetskaya, Irina V.
dc.contributor.authorHeygster, Georg
dc.contributor.authorKunkel, Daniel
dc.contributor.authorMaturilli, Marion
dc.contributor.authorMech, Mario
dc.contributor.authorViceto, Carolina
dc.contributor.authorRinke, Annette
dc.contributor.authorSchmithüsen, Holger
dc.contributor.authorEhrlich, André
dc.contributor.authorMacke, Andreas
dc.contributor.authorLüpkes, Christof
dc.contributor.authorWendisch, Manfred
dc.date.accessioned2023-04-13T08:40:06Z
dc.date.available2023-04-13T08:40:06Z
dc.date.issued2018
dc.description.abstractThe 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 <span classCombining double low line"inline-formula 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.eng
dc.description.versionpublishedVersioneng
dc.identifier.urihttps://oa.tib.eu/renate/handle/123456789/11934
dc.identifier.urihttp://dx.doi.org/10.34657/10967
dc.language.isoeng
dc.publisherKatlenburg-Lindau : EGU
dc.relation.doihttps://doi.org/10.5194/acp-18-17995-2018
dc.relation.essn1680-7324
dc.relation.ispartofseriesAtmospheric Chemistry and Physics 18 (2018), Nr. 24eng
dc.rights.licenseCC BY 4.0 Unported
dc.rights.urihttps://creativecommons.org/licenses/by/4.0
dc.subjectadvectioneng
dc.subjectcloud covereng
dc.subjectcloud microphysicseng
dc.subjectmeteorologyeng
dc.subjectsummereng
dc.subjectsynoptic meteorologyeng
dc.subjectArcticeng
dc.subjectSvalbardeng
dc.subjectSvalbard and Jan Mayeneng
dc.subject.ddc550
dc.titleMeteorological conditions during the ACLOUD/PASCAL field campaign near Svalbard in early summer 2017eng
dc.typearticle
dc.typeText
dcterms.bibliographicCitation.journalTitleAtmospheric Chemistry and Physics
tib.accessRightsopenAccess
wgl.contributorTROPOS
wgl.subjectGeowissenschaftenger
wgl.typeZeitschriftenartikelger
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