CRAAS: A European Cloud Regime dAtAset Based on the CLAAS-2.1 Climate Data Record

dc.bibliographicCitation.firstPage5548
dc.bibliographicCitation.issue21
dc.bibliographicCitation.volume14
dc.contributor.authorTzallas, Vasileios
dc.contributor.authorHünerbein, Anja
dc.contributor.authorStengel, Martin
dc.contributor.authorMeirink, Jan Fokke
dc.contributor.authorBenas, Nikos
dc.contributor.authorTrentmann, Jörg
dc.contributor.authorMacke, Andreas
dc.date.accessioned2023-03-01T09:28:11Z
dc.date.available2023-03-01T09:28:11Z
dc.date.issued2022
dc.description.abstractGiven the important role of clouds in our planet’s climate system, it is crucial to further improve our understanding of their governing processes as well as the resulting spatio-temporal variability of their properties. This co-variability of different cloud optical properties is adequately represented through the well-established concept of cloud regimes. The focus of the present study lies on the creation of a cloud regime dataset over Europe, named “Cloud Regime dAtAset based on the CLAAS-2.1 climate data record” (CRAAS), in order to analyze their variability and their changes at different spatio-temporal scales. In addition, co-occurrences between the cloud regimes and large-scale weather patterns are investigated. The CLoud property dAtAset using Spinning Enhanced Visible and Infrared (SEVIRI) edition 2.1 (CLAAS-2.1) data record, which is produced by the Satellite Application Facility on Climate Monitoring (CM SAF), was used as the basis for the derivation of the cloud regimes over Europe for a 14-year period (2004–2017). In particular, the cloud optical thickness (COT) and cloud top pressure (CTP) products of CLAAS-2.1 were used in order to compute 2D histograms. Then, the k-means clustering algorithm was applied to the generated 2D histograms in order to derive the cloud regimes. Eight cloud regimes were identified, which, along with the geographical distribution of their frequency of occurrence, assisted in providing a detailed description of the climate of the cloud properties over Europe. The annual and diurnal variabilities of the eight cloud regimes were studied, and trends in their frequency of occurrence were also examined. Larger changes in the frequency of occurrence of the produced cloud regimes were found for a regime associated to alto- and nimbo-type clouds and for a regime connected to shallow cumulus clouds and fog (−0.65% and +0.70% for the time period of the study, respectively).eng
dc.description.versionpublishedVersioneng
dc.identifier.urihttps://oa.tib.eu/renate/handle/123456789/11605
dc.identifier.urihttp://dx.doi.org/10.34657/10638
dc.language.isoeng
dc.publisherBasel : MDPI
dc.relation.doihttps://doi.org/10.3390/rs14215548
dc.relation.essn2072-4292
dc.relation.ispartofseriesRemote sensing 14 (2022), Nr. 21eng
dc.rights.licenseCC BY 4.0 Unported
dc.rights.urihttps://creativecommons.org/licenses/by/4.0
dc.subjectclimateeng
dc.subjectcloud regimeseng
dc.subjectCRAASeng
dc.subjectEuropeeng
dc.subjectvariabilityeng
dc.subjectweather typeseng
dc.subject.ddc620
dc.titleCRAAS: A European Cloud Regime dAtAset Based on the CLAAS-2.1 Climate Data Recordeng
dc.typearticle
dc.typeText
dcterms.bibliographicCitation.journalTitleRemote sensing
tib.accessRightsopenAccess
wgl.contributorTROPOS
wgl.subjectIngenieurwissenschaftenger
wgl.typeZeitschriftenartikelger
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