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dc.contributor.authorBerx, Barbara
dc.contributor.authorVolkov, Denis
dc.contributor.authorBaehr, Johanna
dc.contributor.authorBaringer, Molly O.
dc.contributor.authorBurmeister, Kristin
dc.contributor.authorCunningham, Stuart
dc.contributor.authorDe Jong, Marieke Femke
dc.contributor.authorde Steur, Laura
dc.contributor.authorDong, Shenfu
dc.contributor.authorFrajka-Williams, Eleanor
dc.contributor.authorGoni, Gustavo J.
dc.contributor.authorHolliday, N. Penny
dc.contributor.authorHummels, Rebecca
dc.contributor.authorIngvaldsen, Randi Brunvær
dc.contributor.authorJochumsen, Kerstin
dc.contributor.authorJohns, William
dc.contributor.authorJónsson, Steingrímur
dc.contributor.authorKieke, Dagmar
dc.contributor.authorKrishfield, Richard
dc.contributor.authorLankhorst, Matthias
dc.contributor.authorLarsen, Karin Margetha H.
dc.contributor.authorLe Bras, Isabela
dc.contributor.authorLee, Craig M.
dc.contributor.authorLi, Feili
dc.contributor.authorMacrander, Andreas
dc.contributor.authorMcCarthy, Gerard
dc.contributor.authorMoat, Ben I.
dc.contributor.authorMoritz, Martin
dc.contributor.authorPerez, Renellys C.
dc.contributor.authorPolyakov, Igor
dc.contributor.authorProshutinsky, Andrey
dc.contributor.authorRabe, Berit
dc.contributor.authorRhein, Monika
dc.contributor.authorSchmid, Claudia
dc.contributor.authorSkagseth, Øystein
dc.contributor.authorSmeed, David A.
dc.contributor.authorTimmermans, Mary-Louise
dc.contributor.authorvon Appen, Wilken-Jon
dc.contributor.authorWilliams, Bill
dc.contributor.authorWoodgate, Rebecca
dc.contributor.authorYashayaev, Igor
dc.contributor.authorBrandt, Peter
dc.contributor.authorLozier, Susan
dc.contributor.authorMertens, Christian
dc.contributor.authorKarstensen, Johannes
dc.date.accessioned2022-03-02T11:47:39Z
dc.date.available2022-03-02T11:47:39Z
dc.date.created2022-02-11T20:17:32Z
dc.date.issued2021
dc.identifier.citationOceanography. 2021, 34 (4), 10-11.en_US
dc.identifier.issn1042-8275
dc.identifier.urihttps://hdl.handle.net/11250/2982446
dc.description.abstractOcean circulation redistributes heat, freshwater, carbon, and nutrients all around the globe. Because of their importance in regulating climate, weather, extreme events, sea level, fisheries, and ecosystems, large-scale ocean currents should be monitored continuously. The Atlantic is unique as the only ocean basin where heat is, on average, transported northward in both hemispheres as part of the Atlantic Meridional Overturning Circulation (AMOC). The largely unrestricted connection with the Arctic and Southern Oceans allows ocean currents to exchange heat, freshwater, and other properties with polar latitudes.en_US
dc.language.isoengen_US
dc.titleClimate-Relevant Ocean Transport Measurements in the Atlantic and Arctic Oceansen_US
dc.typePeer revieweden_US
dc.typeJournal articleen_US
dc.description.versionpublishedVersionen_US
dc.source.pagenumber10-11en_US
dc.source.volume34en_US
dc.source.journalOceanographyen_US
dc.source.issue4en_US
dc.identifier.doi10.5670/oceanog.2021.supplement.02-04
dc.identifier.cristin2000702
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode1


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