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dc.contributor.authorJ. T. Pasquier
dc.contributor.authorR. O. David
dc.contributor.authorG. Freitas
dc.contributor.authorR. Gierens
dc.contributor.authorY. Gramlich
dc.contributor.authorS. Haslett
dc.contributor.authorG. Li
dc.contributor.authorB. Schäfer
dc.contributor.authorK. Siegel
dc.contributor.authorJ. Wieder
dc.contributor.authorK. Adachi
dc.contributor.authorF. Belosi
dc.contributor.authorT. Carlsen
dc.contributor.authorS. Decesari
dc.contributor.authorK. Ebell
dc.contributor.authorS. Gilardoni
dc.contributor.authorM. Gysel-Beer
dc.contributor.authorJ. Henneberger
dc.contributor.authorJ. Inoue
dc.contributor.authorZ. A. Kanji
dc.contributor.authorM. Koike
dc.contributor.authorY
dc.date.accessioned2023-04-12T18:50:32Z
dc.date.available2023-04-12T18:50:32Z
dc.date.copyright2022/11/14
dc.date.issued2022
dc.identifier.otherBAMS-D-21-0034.1.pdf
dc.identifier.urihttp://yetl.yabesh.ir/yetl1/handle/yetl/4290335
dc.description.abstractThe Arctic is warming at more than twice the rate of the global average. This warming is influenced by clouds, which modulate the solar and terrestrial radiative fluxes and, thus, determine the surface energy budget. However, the interactions among clouds, aerosols, and radiative fluxes in the Arctic are still poorly understood. To address these uncertainties, the Ny-Ålesund Aerosol Cloud Experiment (NASCENT) study was conducted from September 2019 to August 2020 in Ny-Ålesund, Svalbard. The campaign’s primary goal was to elucidate the life cycle of aerosols in the Arctic and to determine how they modulate cloud properties throughout the year. In situ and remote sensing observations were taken on the ground at sea level, at a mountaintop station, and with a tethered balloon system. An overview of the meteorological and the main aerosol seasonality encountered during the NASCENT year is introduced, followed by a presentation of first scientific highlights. In particular, we present new findings on aerosol physicochemical and molecular properties. Further, the role of cloud droplet activation and ice crystal nucleation in the formation and persistence of mixed-phase clouds, and the occurrence of secondary ice processes, are discussed and compared to the representation of cloud processes within the regional Weather Research and Forecasting Model. The paper concludes with research questions that are to be addressed in upcoming NASCENT publications.
dc.publisherAmerican Meteorological Society
dc.titleThe Ny-Ålesund Aerosol Cloud Experiment (NASCENT): Overview and First Results
dc.typeJournal Paper
dc.journal.volume103
dc.journal.issue11
dc.journal.titleBulletin of the American Meteorological Society
dc.identifier.doi10.1175/BAMS-D-21-0034.1
dc.journal.fristpageE2533
dc.journal.lastpageE2558
dc.pageE2533–E2558
dc.treeBulletin of the American Meteorological Society:;2022:;volume( 103 ):;issue: 011
dc.contenttypeFulltext


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