Reduction in meridional heat export contributes to recent Indian Ocean warming
Reduction in meridional heat export contributes to recent Indian Ocean warming
Since 2000, the Indian Ocean has warmed more rapidly than the Atlantic or Pacific Oceans. Air–sea fluxes alone cannot explain the rapid Indian Ocean warming, which has so far been linked to an increase in temperature transport into the basin through the Indonesian Throughflow (ITF). Here, we investigate the role that the heat transport out of the basin at 36°S plays in the warming. Adding the heat transport out of the basin to the ITF temperature transport into the basin, we calculate the decadal mean Indian Ocean heat budget over the 2010s. We find that heat convergence increased within the Indian Ocean over 2000–19. The heat convergence over the 2010s is of the same order as the warming rate, and thus the net air–sea fluxes are near zero. This is a significant change from previous analyses using transbasin hydrographic sections from 1987, 2002, and 2009, which all found divergences of heat. A 2-yr time series shows that seasonal aliasing is not responsible for the decadal change. The anomalous ocean heat convergence over the 2010s in comparison with previous estimates is due to changes in ocean currents at both the southern boundary (33%) and the ITF (67%). We hypothesize that the changes at the southern boundary are linked to an observed broadening of the Agulhas Current, implying that temperature and velocity data at the western boundary are crucial to constrain heat budget changes.
329–345
McMonigal, K
b83796dd-b4ef-467d-9c03-f1da7df3a0f4
Gunn, Kathryn
5952c101-ecf3-4b62-b817-86007cdc8ce4
Beal, Lisa M
c563d2af-6b98-4e76-9f73-d3bac64501c7
Elipot, Shane
c298217e-deac-444a-bf05-ef02bc6dd923
Willis, Josh
89277327-5a02-4e95-9412-cb5a912abf44
1 March 2022
McMonigal, K
b83796dd-b4ef-467d-9c03-f1da7df3a0f4
Gunn, Kathryn
5952c101-ecf3-4b62-b817-86007cdc8ce4
Beal, Lisa M
c563d2af-6b98-4e76-9f73-d3bac64501c7
Elipot, Shane
c298217e-deac-444a-bf05-ef02bc6dd923
Willis, Josh
89277327-5a02-4e95-9412-cb5a912abf44
McMonigal, K, Gunn, Kathryn, Beal, Lisa M, Elipot, Shane and Willis, Josh
(2022)
Reduction in meridional heat export contributes to recent Indian Ocean warming.
Journal of Physical Oceanography, .
(doi:10.1175/jpo-d-21-0085.1).
Abstract
Since 2000, the Indian Ocean has warmed more rapidly than the Atlantic or Pacific Oceans. Air–sea fluxes alone cannot explain the rapid Indian Ocean warming, which has so far been linked to an increase in temperature transport into the basin through the Indonesian Throughflow (ITF). Here, we investigate the role that the heat transport out of the basin at 36°S plays in the warming. Adding the heat transport out of the basin to the ITF temperature transport into the basin, we calculate the decadal mean Indian Ocean heat budget over the 2010s. We find that heat convergence increased within the Indian Ocean over 2000–19. The heat convergence over the 2010s is of the same order as the warming rate, and thus the net air–sea fluxes are near zero. This is a significant change from previous analyses using transbasin hydrographic sections from 1987, 2002, and 2009, which all found divergences of heat. A 2-yr time series shows that seasonal aliasing is not responsible for the decadal change. The anomalous ocean heat convergence over the 2010s in comparison with previous estimates is due to changes in ocean currents at both the southern boundary (33%) and the ITF (67%). We hypothesize that the changes at the southern boundary are linked to an observed broadening of the Agulhas Current, implying that temperature and velocity data at the western boundary are crucial to constrain heat budget changes.
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Published date: 1 March 2022
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Local EPrints ID: 484096
URI: http://eprints.soton.ac.uk/id/eprint/484096
ISSN: 0022-3670
PURE UUID: 55e07bb6-7a0f-48fe-ad33-4ad96e1521a3
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Date deposited: 09 Nov 2023 18:19
Last modified: 18 Mar 2024 04:16
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Author:
K McMonigal
Author:
Kathryn Gunn
Author:
Lisa M Beal
Author:
Shane Elipot
Author:
Josh Willis
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