Heat and turbulent kinetic energy budgets for surface layer cooling induced by the passage of Hurricane Frances (2004)

• Published in: Journal of Geophysical Research. B. Solid Earth 2009-12, Vol.114 (C12), p.n/a
• Main Authors: Huang, Peisheng, Sanford, Thomas B., Imberger, Jörg
• Format: Article
• Language: English
• Subjects: Aerodynamics; air-sea interaction; Computational fluid dynamics; Earth sciences; Earth, ocean, space; Exact sciences and technology; Floats; Free surfaces; Geophysics; Heat exchange; Hurricanes; Kinetic energy; Marine; oceanic mixing; Physical oceanography; Potential energy; Precipitation; sea surface cooling; Sea surface temperature; Surface layer; Surface water; Turbulence
• ISSN: 0148-0227; 2169-9275; 2156-2202; 2169-9291
• DOI: 10.1029/2009JC005603

Heat and turbulent kinetic energy budgets of the ocean surface layer during the passage of Hurricane Frances were examined using a three‐dimensional hydrodynamic model. In situ data obtained with the Electromagnetic‐Autonomous Profiling Explorer (EM‐APEX) floats were used to set up the initial conditions of the model simulation and to compare to the simulation results. The spatial heat budgets reveal that during the hurricane passage, not only the entrainment in the bottom of surface mixed layer but also the horizontal water advection were important factors determining the spatial pattern of sea surface temperature. At the free surface, the hurricane‐brought precipitation contributed a negligible amount to the air‐sea heat exchange, but the precipitation produced a negative buoyancy flux in the surface layer that overwhelmed the instability induced by the heat loss to the atmosphere. Integrated over the domain within 400 km of the hurricane eye on day 245.71 of 2004, the rate of heat anomaly in the surface water was estimated to be about 0.45 PW (1 PW = 1015 W), with about 20% (0.09 PW in total) of this was due to the heat exchange at the air‐sea interface, and almost all the remainder (0.36 PW) was downward transported by oceanic vertical mixing. Shear production was the major source of turbulent kinetic energy amounting 88.5% of the source of turbulent kinetic energy, while the rest (11.5%) was attributed to the wind stirring at sea surface. The increase of ocean potential energy due to vertical mixing represented 7.3% of the energy deposited by wind stress.