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{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2023,9,11]],"date-time":"2023-09-11T21:17:09Z","timestamp":1694467029854},"reference-count":100,"publisher":"Wiley","issue":"755","license":[{"start":{"date-parts":[[2023,6,19]],"date-time":"2023-06-19T00:00:00Z","timestamp":1687132800000},"content-version":"vor","delay-in-days":0,"URL":"http:\/\/creativecommons.org\/licenses\/by\/4.0\/"}],"funder":[{"DOI":"10.13039\/501100001659","name":"Deutsche Forschungsgemeinschaft","doi-asserted-by":"publisher","award":["268020496"]}],"content-domain":{"domain":["rmets.onlinelibrary.wiley.com"],"crossmark-restriction":true},"short-container-title":["Quart J Royal Meteoro Soc"],"published-print":{"date-parts":[[2023,7]]},"abstract":"<jats:title>Abstract<\/jats:title><jats:p>The Arctic near\u2010surface air temperature increases most strongly during the cold season, and ocean heat storage has often been cited as a crucial component in linking the ice\u2010albedo radiative feedback, which is active in summer, and near\u2010surface air temperature increase in winter, when the lapse rate feedback contributes to Arctic warming. Here, we first estimate how much local heat storage and ocean heat transport contribute to net surface energy fluxes on a seasonal scale in CMIP6 models. We then compare contributions in a base state under weak anthropogenic forcing to a near\u2010present\u2010day state in which significant Arctic amplification is simulated. Our analysis indicates that, in a few regions, ocean heat transport plays a larger role for cold\u2010season net surface energy fluxes compared with local heat storage. Analyzing differences between past and near\u2010present\u2010day conditions suggests that the lapse rate feedback, which mainly acts during the cold season in warm water inflow regions, may be more strongly influenced than previously thought by increased ocean heat transport from lower latitudes.<\/jats:p>","DOI":"10.1002\/qj.4496","type":"journal-article","created":{"date-parts":[[2023,5,29]],"date-time":"2023-05-29T12:03:57Z","timestamp":1685361837000},"page":"2091-2106","update-policy":"http:\/\/dx.doi.org\/10.1002\/crossmark_policy","source":"Crossref","is-referenced-by-count":0,"title":["Relative contributions of local heat storage and ocean heat transport to cold\u2010season Arctic Ocean surface energy fluxes in CMIP6 models"],"prefix":"10.1002","volume":"149","author":[{"given":"Khaled al","family":"Hajjar","sequence":"first","affiliation":[{"name":"Institute for Meteorology Leipzig University Leipzig Germany"}]},{"ORCID":"http:\/\/orcid.org\/0000-0002-3987-2303","authenticated-orcid":false,"given":"Marc","family":"Salzmann","sequence":"additional","affiliation":[{"name":"Institute for Meteorology Leipzig University Leipzig Germany"}]}],"member":"311","published-online":{"date-parts":[[2023,6,19]]},"reference":[{"key":"e_1_2_6_2_1","doi-asserted-by":"publisher","DOI":"10.1175\/JCLI-D-11-00466.1"},{"key":"e_1_2_6_3_1","doi-asserted-by":"publisher","DOI":"10.1029\/2019jc016036"},{"key":"e_1_2_6_4_1","doi-asserted-by":"publisher","DOI":"10.1029\/2019GL086706"},{"key":"e_1_2_6_5_1","doi-asserted-by":"publisher","DOI":"10.1071\/ES19040"},{"key":"e_1_2_6_6_1","doi-asserted-by":"publisher","DOI":"10.1029\/2020GL091109"},{"key":"e_1_2_6_7_1","unstructured":"Boucher O. Denvil S. Levavasseur G. Cozic A. Caubel A. Foujols M.\u2010A. Meurdesoif Y. Cadule P. Devilliers M. Dupont E.andLurton T.(2019)IPSL IPSL\u2010CM6A\u2010LR model output prepared for CMIP6 ScenarioMIP ssp245.Versions 20190119 20190516 20191121 20191003 20200218."},{"key":"e_1_2_6_8_1","unstructured":"Boucher O. Denvil S. Levavasseur G. Cozic A. Caubel A. Foujols M.\u2010A. Meurdesoif Y. Cadule P. Devilliers M. Ghattas J. Lebas N. Lurton T. Mellul L. Musat I. Mignot J.andCheruy F.(2018)IPSL IPSL\u2010CM6A\u2010LR model output prepared for CMIP6 CMIP historical.Versions 20180803 20190802\u201320211229."},{"key":"e_1_2_6_9_1","doi-asserted-by":"publisher","DOI":"10.1029\/2019MS002010"},{"key":"e_1_2_6_10_1","unstruct
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