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Southern Ocean carbon sink enhanced by sea-ice feedbacks at the Antarctic Cold Reversal Nature Geoscience: 10, 2020
(Ref: 16273)
Authors:
Fogwill C.J.Turney C.S.M.Menviel L.Baker A.Weber M.E.Ellis B.Thomas Z.A.Golledge N.R.Etheridge D.Rubino M.Thornton D.P.van Ommen T. D.Moy A.D.Curran M. A. J.Davies S.Bird M.I.Munksgaard N.C.Rootes C.M.Millman H.Vohra J.Rivera A.Mackintosh A.Pike J.Hall I.R.Bagshaw E.A.Rainsley E.Bronk-Ramsey C.Montenari M.Cage A.G.Harris M.R.P.Jones R.Power A.Love J.Young J.Weyrich L.S.Cooper A.
Category 1: Peer-reviewed literature
Antarctic ice sheet discharge driven by atmosphere-ocean feedbacks at the Last Glacial Termination Scientific Reports, 2017
(Ref: 16062)
Authors:
Category 1: Peer-reviewed literature
Quasi-Stationary Rossby Waves in the Southern Extratropics: An Examination of Meteorological Reanalyses and Climate Model Simulations. Stratosphere-troposphere Processes and their Role in Climate (SPARC) 2014 General Assembly, Queenstown, New Zealand, 12-17 January 2014, 2014
(Ref: 15170)
Authors:
Category 3: Poster
Large-scale zonal asymmetries in the climatological spatial pattern of atmospheric variables such as geopotential height, temperature, and trace gas concentration are primarily dictated by the characteristics of quasi-stationary Rossby waves (QSWs).