Please use this identifier to cite or link to this item: http://doi.org/10.25358/openscience-9245
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dc.contributor.authorMoser, Manuel-
dc.contributor.authorVoigt, Christiane-
dc.contributor.authorJurkat-Witschas, Tina-
dc.contributor.authorHahn, Valerian-
dc.contributor.authorMioche, Guillaume-
dc.contributor.authorJourdan, Olivier-
dc.contributor.authorDupuy, Régis-
dc.contributor.authorGourbeyre, Christophe-
dc.contributor.authorSchwarzenboeck, Alfons-
dc.contributor.authorLucke, Johannes-
dc.contributor.authorBoose, Yvonne-
dc.contributor.authorMech, Mario-
dc.contributor.authorBorrmann, Stephan-
dc.contributor.authorEhrlich, André-
dc.contributor.authorHerber, Andreas-
dc.contributor.authorLüpkes, Christof-
dc.contributor.authorWendisch, Manfred-
dc.date.accessioned2023-07-03T06:25:22Z-
dc.date.available2023-07-03T06:25:22Z-
dc.date.issued2023-
dc.identifier.urihttps://openscience.ub.uni-mainz.de/handle/20.500.12030/9262-
dc.description.abstractAirborne in situ cloud measurements were carried out over the northern Fram Strait between Greenland and Svalbard in spring 2019 and summer 2020. In total, 811 min of low-level cloud observations were performed during 20 research flights above the sea ice and the open Arctic ocean with the Polar 5 research aircraft of the Alfred Wegener Institute. Here, we combine the comprehensive in situ cloud data to investigate the distributions of particle number concentration N, effective diameter Deff, and cloud water content CWC (liquid and ice) of Arctic clouds below 500 m altitude, measured at latitudes between 76 and 83◦ N. We developed a method to quantitatively derive the occurrence probability of their thermodynamic phase from the combination of microphysical cloud probe and Polar Nephelometer data. Finally, we assess changes in cloud microphysics and cloud phase related to ambient meteorological conditions in spring and summer and address effects of the sea ice and open-ocean surface conditions. We find median N from 0.2 to 51.7 cm−3 and about 2 orders of magnitude higher N for mainly liquid clouds in summer compared to ice and mixed-phase clouds measured in spring. A southerly flow from the sea ice in cold air outbreaks dominates cloud formation processes at temperatures mostly below −10 ◦C in spring, while northerly warm air intrusions favor the formation of liquid clouds at warmer temperatures in summer. Our results show slightly higher N in clouds over the sea ice compared to the open ocean, indicating enhanced cloud formation processes over the sea ice. The median CWC is higher in summer (0.16 gm−3 ) than in spring (0.06 gm−3 ), as this is dominated by the available atmospheric water content and the temperatures at cloud formation level. We find large differences in the particle sizes in spring and summer and an impact of the surface conditions, which modifies the heat and moisture fluxes in the boundary layer. By combining microphysical cloud data with thermodynamic phase information from the Polar Nephelometer, we find mixed-phase clouds to be the dominant thermodynamic cloud phase in spring, with a frequency of occurrence of 61 % over the sea ice and 66 % over the ocean. Pure ice clouds exist almost exclusively over the open ocean in spring, and in summer the cloud particles are most likely in the liquid water state.en_GB
dc.language.isoengde
dc.rightsCC BY*
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/*
dc.subject.ddc530 Physikde_DE
dc.subject.ddc530 Physicsen_GB
dc.subject.ddc540 Chemiede_DE
dc.subject.ddc540 Chemistry and allied sciencesen_GB
dc.subject.ddc550 Geowissenschaftende_DE
dc.subject.ddc550 Earth sciencesen_GB
dc.titleMicrophysical and thermodynamic phase analyses of Arctic low-level clouds measured above the sea ice and the open ocean in spring and summeren_GB
dc.typeZeitschriftenaufsatzde
dc.identifier.doihttp://doi.org/10.25358/openscience-9245-
jgu.type.contenttypeScientific articlede
jgu.type.dinitypearticleen_GB
jgu.type.versionPublished versionde
jgu.type.resourceTextde
jgu.organisation.departmentFB 09 Chemie, Pharmazie u. Geowissensch.de
jgu.organisation.number7950-
jgu.organisation.nameJohannes Gutenberg-Universität Mainz-
jgu.rights.accessrightsopenAccess-
jgu.journal.titleAtmospheric Chemistry and Physicsde
jgu.journal.volume23.2023de
jgu.pages.start7257de
jgu.pages.end7280de
jgu.pages.alternativeacp-23-7257-2023de
jgu.publisher.year2023-
jgu.publisher.nameCopernicus GmbH EGUde
jgu.publisher.placeKatlenburg-Lindaude
jgu.publisher.issn1680-7324de
jgu.organisation.placeMainz-
jgu.subject.ddccode530de
jgu.subject.ddccode540de
jgu.subject.ddccode550de
jgu.publisher.doi10.5194/acp-23-7257-2023de
jgu.organisation.rorhttps://ror.org/023b0x485-
jgu.subject.dfgNaturwissenschaftende
Appears in collections:DFG-491381577-G

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