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contributor authorLatif, M.
contributor authorBöning, C.
contributor authorWillebrand, J.
contributor authorBiastoch, A.
contributor authorDengg, J.
contributor authorKeenlyside, N.
contributor authorSchweckendiek, U.
contributor authorMadec, G.
date accessioned2017-06-09T17:02:22Z
date available2017-06-09T17:02:22Z
date copyright2006/09/01
date issued2006
identifier issn0894-8755
identifier otherams-78342.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4221001
description abstractAnalyses of ocean observations and model simulations suggest that there have been considerable changes in the thermohaline circulation (THC) during the last century. These changes are likely to be the result of natural multidecadal climate variability and are driven by low-frequency variations of the North Atlantic Oscillation (NAO) through changes in Labrador Sea convection. Indications of a sustained THC weakening are not seen during the last few decades. Instead, a strengthening since the 1980s is observed. The combined assessment of ocean hydrography data and model results indicates that the expected anthropogenic weakening of the THC will remain within the range of natural variability during the next several decades.
publisherAmerican Meteorological Society
titleIs the Thermohaline Circulation Changing?
typeJournal Paper
journal volume19
journal issue18
journal titleJournal of Climate
identifier doi10.1175/JCLI3876.1
journal fristpage4631
journal lastpage4637
treeJournal of Climate:;2006:;volume( 019 ):;issue: 018
contenttypeFulltext


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