Mechanisms of Heat Content and Thermocline Change in the Subtropical and Subpolar North Atlantic

Williams, Richard G ORCID: 0000-0002-3180-7558, Roussenov, Vassil ORCID: 0000-0003-4128-9712, Lozier, M Susan and Smith, Doug
(2015) Mechanisms of Heat Content and Thermocline Change in the Subtropical and Subpolar North Atlantic. JOURNAL OF CLIMATE, 28 (24). pp. 9803-9815.

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<jats:title>Abstract</jats:title> <jats:p>In the North Atlantic, there are pronounced gyre-scale changes in ocean heat content on interannual-to-decadal time scales, which are associated with changes in both sea surface temperature and thermocline thickness; the subtropics are often warm with a thick thermocline when the subpolar gyre is cool with a thin thermocline, and vice versa. This climate variability is investigated using a semidiagnostic dynamical analysis of historical temperature and salinity data from 1962 to 2011 together with idealized isopycnic model experiments. On time scales of typically 5 yr, the tendencies in upper-ocean heat content are not simply explained by the area-averaged atmospheric forcing for each gyre but instead dominated by heat convergences associated with the meridional overturning circulation. In the subtropics, the most pronounced warming events are associated with an increased influx of tropical heat driven by stronger trade winds. In the subpolar gyre, the warming and cooling events are associated with changes in western boundary density, where increasing Labrador Sea density leads to an enhanced overturning and an influx of subtropical heat. Thus, upper-ocean heat content anomalies are formed in a different manner in the subtropical and subpolar gyres, with different components of the meridional overturning circulation probably excited by the local imprint of atmospheric forcing.</jats:p>

Item Type: Article
Uncontrolled Keywords: Geographic location, entity, North Atlantic Ocean, Circulation, Dynamics, Ekman pumping, transport, Meridional overturning circulation, Thermocline circulation, Atm, Ocean Structure, Phenomena, Gyres, Thermocline
Depositing User: Symplectic Admin
Date Deposited: 11 May 2016 08:49
Last Modified: 19 Jan 2023 07:37
DOI: 10.1175/JCLI-D-15-0097.1
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