The new BELUGA setup for collocated turbulence and radiation measurements using a tethered balloon: First applications in the cloudy Arctic boundary layer

dc.bibliographicCitation.firstPage4019eng
dc.bibliographicCitation.issue7eng
dc.bibliographicCitation.volume12eng
dc.contributor.authorEgerer, U.
dc.contributor.authorGottschalk, M.
dc.contributor.authorSiebert, H.
dc.contributor.authorEhrlich, A.
dc.contributor.authorWendisch, M.
dc.date.accessioned2020-07-13T11:01:23Z
dc.date.available2020-07-13T11:01:23Z
dc.date.issued2019
dc.description.abstractThe new BELUGA (Balloon-bornE moduLar Utility for profilinG the lower Atmosphere) tethered balloon system is introduced. It combines a set of instruments to measure turbulent and radiative parameters and energy fluxes. BELUGA enables collocated measurements either at a constant altitude or as vertical profiles up to 1.5km in height. In particular, the instrument payload of BELUGA comprises three modular instrument packages for high-resolution meteorological, wind vector and broadband radiation measurements. Collocated data acquisition allows for estimates of the driving parameters in the energy balance at various heights. Heating rates and net irradiances can be related to turbulent fluxes and local turbulence parameters such as dissipation rates. In this paper the technical setup, the instrument performance, and the measurement strategy of BELUGA are explained. Furthermore, the high vertical resolution due to the slow ascent speed is highlighted as a major advantage of tethered balloon-borne observations. Three illustrative case studies of the first application of BELUGA in the Arctic atmospheric boundary layer are presented. As a first example, measurements of a single-layer stratocumulus are discussed. They show a pronounced cloud top radiative cooling of up to 6K h-1. To put this into context, a second case elaborates respective measurements with BELUGA in a cloudless situation. In a third example, a multilayer stratocumulus was probed, revealing reduced turbulence and negligible cloud top radiative cooling for the lower cloud layer. In all three cases the net radiative fluxes are much higher than turbulent fluxes. Altogether, BELUGA has proven its robust performance in cloudy conditions of the Arctic atmospheric boundary layer.eng
dc.description.sponsorshipLeibniz_Fondseng
dc.description.versionpublishedVersioneng
dc.identifier.urihttps://oa.tib.eu/renate/handle/123456789/4921
dc.identifier.urihttps://doi.org/10.34657/3550
dc.language.isoengeng
dc.publisherGöttingen : Copernicus GmbHeng
dc.relation.doihttps://doi.org/10.5194/amt-12-4019-2019
dc.relation.ispartofseriesAtmospheric Measurement Techniques 12 (2019), 7eng
dc.relation.issn1867-1381
dc.rights.licenseCC BY 4.0 Unportedeng
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/eng
dc.subjectballoon observationeng
dc.subjectboundary layereng
dc.subjectcloud covereng
dc.subjectcloud radiative forcingeng
dc.subjectcoolingeng
dc.subjectdata acquisitioneng
dc.subjectdissipationeng
dc.subjectenergy balanceeng
dc.subjectstratocumuluseng
dc.subjectturbulenceeng
dc.subject.ddc550eng
dc.titleThe new BELUGA setup for collocated turbulence and radiation measurements using a tethered balloon: First applications in the cloudy Arctic boundary layereng
dc.typearticleeng
dc.typeTexteng
dcterms.bibliographicCitation.journalTitleAtmospheric Measurement Techniqueseng
tib.accessRightsopenAccesseng
wgl.contributorTROPOSeng
wgl.subjectUmweltwissenschafteneng
wgl.typeZeitschriftenartikeleng
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