Observations indicate that clouds amplify mechanisms of Southern Ocean heat uptake

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dc.contributor.authorMorrison, Ariel L.
dc.contributor.authorSingh, Hansi K.A.
dc.contributor.authorRasch, Philip J.
dc.date.accessioned2022-03-03T23:52:13Z
dc.date.available2022-03-03T23:52:13Z
dc.date.copyright2022en_US
dc.date.issued2022-02-27
dc.descriptionThe authors would like to thank R. Wood and three anonymous reviewers for helpful comments on this manuscript.en_US
dc.description.abstractThe Southern Ocean has absorbed most of the excess heat associated with anthropogenic greenhouse gas emissions. Since Southern Ocean observations are sparse in certain regions and seasons, much of our knowledge of ocean heat uptake is based on climate model simulations. However, climate models still inadequately represent some properties of Southern Ocean clouds, and they have not identified the mechanisms by which clouds may affect Southern Ocean heat uptake (SOHU). Here, we use the ERA5 and JRA-55 reanalyses to assess the influence of clouds and other atmospheric processes on SOHU from 1979 to 2020. We find that years with the highest SOHU between 45° and 65°S are dominated by ocean heat uptake anomalies during winter and spring, but not during summer or fall. Winter and spring cloud cover are up to 7% higher when SOHU is up to 5.5 W/m2 higher than the climatological seasonal mean, with the largest increases in the South Pacific Ocean. Clouds also contain more liquid water. These changes in cloud properties increase downwelling longwave radiation, amplifying ocean heat uptake. Cloud changes are also concomitant with a more stable lower atmosphere, which suppresses turbulent heat fluxes out of the surface. Overall, we find that SOHU is likely not mediated by enhanced surface shortwave absorption over the observational time period. A better understanding of how atmospheric processes impact ocean heat uptake may help improve our understanding of ocean heat uptake mechanisms in the current generation of climate models.en_US
dc.description.reviewstatusRevieweden_US
dc.description.scholarlevelFacultyen_US
dc.description.sponsorshipAriel L. Morrison and Philip J. Rasch were supported by the Regional and Global Model Analysis (RGMA) com-ponent of the Earth and Environmental System Modeling (EESM) program of the U.S. Department of Energy's Office of Science, as contribution to the HiLAT-RASM project. Ariel L. Morrison and Hansi A. Singh were supported by the University of Victoria. This research also used resources of the National Energy Research Scientific Computing (NERSC) Center, a DOE Office of Science User Fa-cility supported by the Office of Science of the U.S. Department of Energy under Contract DE-AC02-05CH11231. The Pacific Northwest National Laboratory is operated for the U.S. Department of Energy by Battelle Memorial Institute un-der contract DE-AC05-76RL01830.en_US
dc.identifier.citationMorrison, A. L., Singh, H. A., & Rasch, P. J. (2022). Observations indicate that clouds amplify mechanisms of Southern Ocean heat uptake. Journal of Geophysical Research: Atmospheres, 127, e2021JD035487. https://doi.org/10.1029/2021JD035487en_US
dc.identifier.urihttps://doi.org/10.1029/2021JD035487
dc.identifier.urihttp://hdl.handle.net/1828/13763
dc.language.isoenen_US
dc.publisherJournal of Geophysical Research: Atmospheresen_US
dc.subjectSouthern oceanen_US
dc.subjectcloudsen_US
dc.subjectocean heat contenten_US
dc.subjectclimateen_US
dc.titleObservations indicate that clouds amplify mechanisms of Southern Ocean heat uptakeen_US
dc.typeArticleen_US

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