Annual cycle observations of aerosols capable of ice formation in central Arctic clouds

dc.contributor.authorCreamean, Jessie M.
dc.contributor.authorBarry, Kevin
dc.contributor.authorHill, Thomas C. J.
dc.contributor.authorHume, Carson
dc.contributor.authorDeMott, Paul J.
dc.contributor.authorShupe, Matthew D.
dc.contributor.authorDahlke, Sandro
dc.contributor.authorWillmes, Sascha
dc.contributor.authorSchmale, Julia
dc.contributor.authorBeck, Ivo
dc.contributor.authorHoppe, Clara J. M.
dc.contributor.authorFong, Allison
dc.contributor.authorChamberlain, Emelia
dc.contributor.authorBowman, Jeff
dc.contributor.authorScharien, Randall K.
dc.contributor.authorPersson, Ola
dc.date.accessioned2023-01-04T22:21:21Z
dc.date.available2023-01-04T22:21:21Z
dc.date.copyright2022en_US
dc.date.issued2022
dc.description.abstractThe Arctic is warming faster than anywhere else on Earth, prompting glacial melt, permafrost thaw, and sea ice decline. These severe consequences induce feedbacks that contribute to amplified warming, affecting weather and climate globally. Aerosols and clouds play a critical role in regulating radiation reaching the Arctic surface. However, the magnitude of their effects is not adequately quantified, especially in the central Arctic where they impact the energy balance over the sea ice. Specifically, aerosols called ice nucleating particles (INPs) remain understudied yet are necessary for cloud ice production and subsequent changes in cloud lifetime, radiative effects, and precipitation. Here, we report observations of INPs in the central Arctic over a full year, spanning the entire sea ice growth and decline cycle. Further, these observations are size-resolved, affording valuable information on INP sources. Our results reveal a strong seasonality of INPs, with lower concentrations in the winter and spring controlled by transport from lower latitudes, to enhanced concentrations of INPs during the summer melt, likely from marine biological production in local open waters. This comprehensive characterization of INPs will ultimately help inform cloud parameterizations in models of all scales.en_US
dc.description.reviewstatusRevieweden_US
dc.description.scholarlevelFacultyen_US
dc.description.sponsorshipThis work was funded by the DOE ARM and Atmospheric System Research (ASR) programs (DE-AC05-76RL01830, DE-2204 SC0019745, DE-SC0019251, DESC0021341) for J.M.C., K.B., T.C.J.H., C.H., P.J.D. and M.D.S.; the U.S. National Science Foundation (NSF) Office of Polar Programs (OPP-1724551) for E.C. and J.B.; and the German Federal Ministry for Education and Research (BMBF) for C.J.M.H. and A.F. through financing the AWI Helmholtz Zentrum für Polar und Meeresforschung and the Polarstern expedition (N-2014-H-060_Dethloff). I.B. received funding from the Swiss National Science Foundation (grant no. 200021_188478). J.S. received funding from the Swiss Polar Institute and holds the Ingvar Kamprad Chair for Extreme Environments Research sponsored by Ferring Pharmaceuticals.en_US
dc.identifier.citationCreamean, J. M., Barry, K., Hill, T. C. J., Hume, C., DeMott, P. J., Shupe, M. D., . . . Persson, O. (2022). “Annual cycle observations of aerosols capable of ice formation in central Arctic clouds.” Nature Communications, 13(3537). https://doi.org/10.1038/s41467-022-31182-xen_US
dc.identifier.urihttps://doi.org/10.1038/s41467-022-31182-x
dc.identifier.urihttp://hdl.handle.net/1828/14618
dc.language.isoenen_US
dc.publisherNature Communicationsen_US
dc.subject.departmentDepartment of Geography
dc.titleAnnual cycle observations of aerosols capable of ice formation in central Arctic cloudsen_US
dc.typeArticleen_US

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