Tracing oceanic sources of heat content available for Atlantic hurricanes
Tracing oceanic sources of heat content available for Atlantic hurricanes
In the Main Development Region (MDR) for Atlantic hurricanes, the volume of water warmer than 26.5°C quantifies the potential source of energy for major storms. Taking a Lagrangian perspective, this warm water is backtracked on seasonal timescales in an eddy-resolving ocean model hindcast spanning 1988–2010. Being confined near the surface and assuming a mixed layer depth of 50 m, net heat fluxes into or out of water parcels advected toward the MDR are inferred from along-trajectory temperature tendencies. To first order, these heat fluxes match surface net heat fluxes during the months over which water advects into the region. Contributions to this warm water in the preceding 6 months include water resident in the MDR (20%–40%), arriving via the North Brazil Current (NBC, 5%–15%), or via Ekman drift across 10°S. In relative terms, decreased contributions from the NBC and Ekman drift and more in situ warming within the MDR lead to warmer, more active hurricane seasons.
Harris, E.A.
29d2058e-dd68-4f5e-995b-0748ff3ef10c
Marsh, R.
b22ef653-0671-46d5-bf81-21c0d6657974
Grist, J.P.
ffea99af-f811-436f-9bac-5b02ba6dc00f
1 May 2023
Harris, E.A.
29d2058e-dd68-4f5e-995b-0748ff3ef10c
Marsh, R.
b22ef653-0671-46d5-bf81-21c0d6657974
Grist, J.P.
ffea99af-f811-436f-9bac-5b02ba6dc00f
Harris, E.A., Marsh, R. and Grist, J.P.
(2023)
Tracing oceanic sources of heat content available for Atlantic hurricanes.
Journal of Geophysical Research: Oceans, 128 (5), [e2022JC019407].
(doi:10.1029/2022JC019407).
Abstract
In the Main Development Region (MDR) for Atlantic hurricanes, the volume of water warmer than 26.5°C quantifies the potential source of energy for major storms. Taking a Lagrangian perspective, this warm water is backtracked on seasonal timescales in an eddy-resolving ocean model hindcast spanning 1988–2010. Being confined near the surface and assuming a mixed layer depth of 50 m, net heat fluxes into or out of water parcels advected toward the MDR are inferred from along-trajectory temperature tendencies. To first order, these heat fluxes match surface net heat fluxes during the months over which water advects into the region. Contributions to this warm water in the preceding 6 months include water resident in the MDR (20%–40%), arriving via the North Brazil Current (NBC, 5%–15%), or via Ekman drift across 10°S. In relative terms, decreased contributions from the NBC and Ekman drift and more in situ warming within the MDR lead to warmer, more active hurricane seasons.
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JGR Oceans - 2023 - Harris - Tracing Oceanic Sources of Heat Content Available for Atlantic Hurricanes
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Accepted/In Press date: 29 March 2023
Published date: 1 May 2023
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Local EPrints ID: 498777
URI: http://eprints.soton.ac.uk/id/eprint/498777
ISSN: 2169-9275
PURE UUID: 1bf9288f-f6c8-4676-87d1-6edfbac21868
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Date deposited: 28 Feb 2025 17:30
Last modified: 01 Mar 2025 02:31
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Author:
R. Marsh
Author:
J.P. Grist
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