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Mechanisms of ocean heat uptake

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dc.contributor.advisor Klinger, Barry A.
dc.contributor.author Garuba, Oluwayemi Anne
dc.creator Garuba, Oluwayemi Anne
dc.date.accessioned 2016-04-19T19:28:50Z
dc.date.available 2016-04-19T19:28:50Z
dc.date.issued 2015
dc.identifier.uri https://hdl.handle.net/1920/10176
dc.description.abstract An important parameter for the climate response to increased greenhouse gases or other radiative forcing is the speed at which heat anomalies propagate downward in the ocean. Ocean heat uptake occurs through passive advection/diffusion of surface heat anomalies and through the redistribution of existing temperature gradients due to circulation changes. Atlantic meridional overturning circulation (AMOC) weakens in a warming climate and this should slow the downward heat advection (compared to a case in which the circulation is unchanged). However, weakening AMOC also causes a deep warming through the redistributive effect, thus increasing the downward rate of heat propagation compared to unchanging circulation. Total heat uptake depends on the combined effect of these two mechanisms.
dc.format.extent 125 pages
dc.language.iso en
dc.rights Copyright 2015 Oluwayemi Anne Garuba
dc.subject Physical oceanography en_US
dc.subject Climate change en_US
dc.subject Atmospheric sciences en_US
dc.subject Climate change en_US
dc.subject Climate transient response en_US
dc.subject Ocean circulation en_US
dc.subject Ocean heat uptake en_US
dc.subject Ocean modelling en_US
dc.title Mechanisms of ocean heat uptake
dc.type Dissertation en
thesis.degree.level Doctoral en
thesis.degree.discipline Climate Dynamics en
thesis.degree.grantor George Mason University en


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