Cite this paper:
ZHANG Lianxin, ZHANG Xuefeng, HAN Guijun, WU Xinrong, CUI Xiaojian, SHAO Caixia, SUN Chunjian, ZHANG Xiaoshuang, WANG Xidong, FU Hongli. Impact of sea spray on upper ocean temperature during typhoon passage: simulation with a 1-D turbulent model[J]. Journal of Oceanology and Limnology, 2015, 33(5): 1164-1180

Impact of sea spray on upper ocean temperature during typhoon passage: simulation with a 1-D turbulent model

ZHANG Lianxin1,2, ZHANG Xuefeng2, HAN Guijun2, WU Xinrong2, CUI Xiaojian2, SHAO Caixia2,3, SUN Chunjian2, ZHANG Xiaoshuang2, WANG Xidong2, FU Hongli2
1 College of Physical and Environmental Oceanography, Ocean University of China, Qingdao 266100, China;
2 Key Laboratory of State Oceanic Administration for Marine Environmental Information Technology, National Marine Data and Information Service, State Oceanic Administration, Tianjin 300171, China;
3 National University of Defense Technology, Changsha 410073, China
Abstract:
At the interface between the lower atmosphere and sea surface, sea spray might significantly influence air-sea heat fluxes and subsequently, modulate upper ocean temperature during a typhoon passage.The effects of sea spray were introduced into the parameterization of sea surface roughness in a 1-D turbulent model, to investigate the effects of sea spray on upper ocean temperature in the Kuroshio Extension area, for the cases of two real typhoons from 2006, Yagi and Soulik.Model output was compared with data from the Kuroshio Extension Observatory (KEO), and Reynolds and AMSRE satellite remote sensing sea surface temperatures.The results indicate drag coefficients that include the spray effect are closer to observations than those without, and that sea spray can enhance the heat fluxes (especially latent heat flux) considerably during a typhoon passage.Consequently, the model results with heat fluxes enhanced by sea spray simulate better the cooling process of the SST and upper-layer temperature profiles.Additionally, results from the simulation of the passage of typhoon Soulik (that passed KEO quickly), which included the sea spray effect, were better than for the simulated passage of typhoon Yagi (that crossed KEO slowly).These promising 1-D results could provide insight into the application of sea spray in general circulation models for typhoon studies.
Key words:    sea spray|upper layer temperature|typhoon|air-sea heat fluxes   
Received: 2014-05-23   Revised: 2014-07-22
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Articles by ZHANG Lianxin
Articles by ZHANG Xuefeng
Articles by HAN Guijun
Articles by WU Xinrong
Articles by CUI Xiaojian
Articles by SHAO Caixia
Articles by SUN Chunjian
Articles by ZHANG Xiaoshuang
Articles by WANG Xidong
Articles by FU Hongli
References:
Andreas E L, DeCosmo J.1999.Sea spray production and influence on air-sea heat and moisture fluxes over the open ocean.Air-Sea Exchange: Physics, Chemistry and Dynamics.In: Geernaert G L ed., Kluwer Academic.p.327-362.
Andreas E L, Emanuel K A.2001.Effects of sea spray on tropical cyclone intensity.J.Atmos.Sci, 58: 3 741-3 751.
Andreas E L, Persson P O G, Hare J E.2008.A bulk turbulent air-sea flux algorithm for high-wind spray conditions.J.Phys.Oceanogr., 38: 1 581-1 596.
Andreas E L.1989.Thermal and size evolution of sea spray droplets.CRREL Rep.89-11.U.S.Army Cold Regions.Research and Engineering Laboratory.37p.
Andreas E L.1990.Time constants for the evolution of sea spray droplets.Tellus B, 42: 481-497.
Andreas E L.1992.Sea spray and the turbulent air-sea heat fluxes.J.Geophys.Res., 97: 11 429-11 441.
Andreas E L.2003.An algorithm to predict the turbulent airsea fluxes in high-wind.spray conditions.Preprints.12th Conference on Interactions of the Sea and Atmosphere.Long Beach.CA, Amer Meteor Soc., 3.4.
Andreas E L.2004.A bulk air-sea flux algorithm for high-wind spray conditions.Version 2.0.Preprints.13th Conference on Interactions of the Sea and Atmosphere.Long Beach,CA, Amer.Meteor Soc., 1.5.
Andreas E L.2010.Spray-mediated enthalpy flux to the atmosphere and salt flux to the ocean in high winds.J.Phys.Oceanogr., 40: 608-619.
Bao J W, Wilczak J M, Choi J K et al.2000.Numerical simulations of air-sea interaction under high wind conditions using a couple model: a study of hurricane development.Mon.Weather.Rev., 128: 2 190-2 210.
Bender M A, Ginis I, Kurihara Y.1993.Numerical simulations of tropical cyclone-ocean interaction with a high-resolution coupled model.J.Geophys.Res., 98 (D12): 23 245-23 262.
Black P G, D'Asaro E A, Drennan W M et al.2007.Air-sea exchange in hurricanes: synthesis of observations from the coupled boundary layer air-sea transfer experiment.Bull.Am.Meteorol Soc., 88 (3): 357-374.
Bortkovskii R S.1987.Air-Sea Exchange of Heat and Moisture during Storms.D.Reidel.194p.
Burchard H, Bolding K, Kühn W, Meister A et al.2006.Description of a flexible and extendable physicalbiogeochemical model system for the water column.J.Mar.Sys., 61: 180-211.
Charnock H.1995.Wind stress on a water surface.Q.J.R.Meteorol.Soc., 81 (350): 639-640.
Donelan M A.1990.Air-Sea Interaction.The Sea: Ocean Engineering Science, 9.In: LeMéhauté B, Hanes D eds.John Wiley and Sons, Inc., New York.p.239-292.
Emanuel K A.1986.An air-sea interaction theory for tropical cyclones.Part I.Steady-state maintenance.J.Atmos.Sci., 43: 585-604.
Emanuel K A.1995.Sensitivity of tropical cyclone to surface exchange coefficient and a revised steady-state model incorporating eye dynamics.J.Atmos.Sci., 52: 3 969-3 976.
Fairall C W, Banner M L, Person W L et al.2009.Investigation of the physical scaling of sea spray spume droplet.J.Geophys Res., 114: C100001, http://dx.doi.org/10.1029/2008JC004918.
Fairall C W, Bradley E F, Rogers D P, Edson J B et al.1996.Bulk parameterization of air-sea fluxes for Tropical Ocean-Global Atmosphere Coupled-Ocean-Atmosphere Experiment.J.Geophys.Res., 101: 3 747-3 764.
Fairall C W, Kepert J D, Holland G J.1994.The effect of sea spray on surface energy transports over the ocean.Global Atmos.Ocean Syst., 2: 121-142.
Iida N, Toba Y, Chaen M.1992.A new expression for the production rate of sea water droplets on the sea surface.J.Oceanogr., 48: 439-460.
Jarosz E, Mitchell D A, Wang D W et al.2007.Bottom-up determination of air-sea momentum exchange under a major tropical cyclone.Science, 315 (5819): 1 707-1 709, http://dx.doi.org/10.1126/science.1136466.
Jeffrey S G, William M F.2008.Effects of sea spray on tropical cyclones simulated under idealized conditions.Mon.Weather.Rev., 136: 1 686-1 705.
Johnson H K, Hojstrup J, Vested H J et al.1998.On the dependence of sea surface roughness on wind waves.J.Phys.Oceanog., 28: 1 702-1 716.
Ling S C, Kao T W, Saad A I.1980.Microdroplets and transport of moisture from ocean.Proc.ASCE J.Eng.Mech.Div., 106: 1 327-1 339.
Liu B, Guan C L, Lian X.2012.The wave state and sea spray related parameterization of wind stress applicable from low to extreme winds.J.Geophys.Res., 117: 1-10.
Liu B.2007.Physical Basis and Numerical Study of the Coupled Atmosphere-Wave Model.PhD Thesis, Ocean University of China.(in Chinese with English abstract)
Liu Z H, Xu J P, Zhu B K et al.2006.Upper ocean to tropical cyclones in northwestern Pacific during 2001-2004 by Argo data.Journal of Tropical Oceanography, 25: 1-8.(in Chinese with English abstract)
Maat N, Kraan C, Oost W A.1991.The roughness of wind waves.Bound Layer Meterol., 54: 89-103.
Makin V K.2005.A note on the drag of the sea surface at hurricane winds.Boundary Layer Meteorol., 115: 169-176.
Masuda A, Kusaba T.1987.On the equilibrium of winds and wind-waves in relation to surface drag.J.Oceanogr.Soc.Jpn, 43: 28-36.
Meirink J F, Makin V K.2001.The impact of sea spray evaporation in a numerical weather prediction model.J.Atmos.Sci., 58 (23): 3 626-3 638.
Monahan E C.1986.The ocean as a source for atmospheric particles.In: Buat-Menard P ed.The Role of Air-Sea Exchange in Geochemical Cycling, D.Reidel Publ.Co.,Dordrecht, Holland.p.129-163.
Monbaliu J.1994.On the use of the Donelan wave spectral parameter as a measure for the roughness of wind waves.Bound Layer Meterol., 67: 277-291.
Perrie W, Andreas E L, Zhang W et al.2005.Sea spray impacts on intensifying midlatitude cyclones.J.Atmos.Sci., 62: 1 867-1 883.
Powell M D, Vickery P J, Reinhold T A.2003.Reduced drag coefficient for high wind speeds in tropical cyclones.Nature, 422: 279-283.
Pruppacher H R, Klett J D.1978.Microphysics of Clouds and Precipitation.D.Reidel, Norwell, Mass.714p.
Riehl H.1954.Tropical Meteorology.McGraw-Hill.392p.
Smith J A.1992.Observed growth of Langmuir circulation.J.Geophys.Res., 97: 5 651-5 664.
Smith M H, Park P M, Consterdine I E.1993.Marine aerosol concentrations and estimated fluxes over the sea.Quart.J.Roy.Meteor.Soc., 119: 809-824.
Toba Y.1972.Local balance in the air-sea boundary process.I.On the growth process of wind waves.J.Oceanogr.Soc.Jpn., 28: 109-120.
Uang C L.1999.Impact of sea spray and oceanic on the development of tropical cyclones.Preprints, 23rd Conference on Hurricanes and Tropical Meteorology,Dallas, TX, Amer.Meteor.Soc.p.30-31.
Umlauf L, Burchard H.2005.Second-order turbulence closure models for geophysics boundary layers.A review of recent work.Cont.Shelf Res., 25: 795-827.
Vickers D, Mahrt L.1997.Fetch limited drag coefficients.Bound Layer Meteorol., 83: 53-79.
Wang Y M, Kepert J D, Holland G J.2001.The effect of sea spray evaporation tropical cyclone boundary layer structure and intensity.Mon.Weather.Rev., 129: 2 481-2 500.
Wu J.1993.Production of spume drops by the wind tearing of wave crests: the search for quantification.J.Geophys.Res., 98: 18 221-18 227.
Yablonsky R M, Ginis I.2009.Limitation of one-dimensional ocean models for coupled hurricane-ocean models forecasts.Mon.Weather Rev., 137: 4 410-4 419.
Zhao D L, Toba Y, Sugioka K et al.2006.New sea spray generation function for spume droplets.J.Geophys.Res., 111 (C2): C02007.1-C02007.11.
Zhao D L.2012.Progress in sea spray and its effects on Air-Sea interaction.Advances in Earth Sciences, 27: 624-632.(in Chinese with English abstract)
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