Role of Ocean Waves in the Coupled Atmosphere-Ocean ... - ecmwf

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Flow separation due to breaking ��f) = � 0(f)(1+b T) dE( k, f , �, x, t) � S dt in � S ds � S nl � S bf
Wind Input – S in dE( k, f , �, x, t) � S dt Donelan, Babanin, Young and Banner (Part I, JTEC, 2005; Part II, JPO, 2006, Part III, JPO, 2007) • a new parameterisation of the wind input function, based on field measurements, is suggested. • the parameterisation includes very strongly forced and steep wave conditions, the wind input for which has never before been directly measured in field conditions. • new physical features of air-sea exchange have been found: - full separation of the air flow at strong wind over steep waves - leads to the sea drag saturation - the exchange mechanism is non-linear and depends on the wave steepness - enhancement of the wind input over breaking waves in � S ds � S nl � S bf
Page 1 and 2: Update on parameterisation of major
Page 3 and 4: Wind Input dE( k, f , �, x, t)
Page 5: The parameterisation dE( k, f , �
Page 9 and 10: Whitecapping Dissipation S ds dE( k
Page 11 and 12: White Cap Dissipation S ds 2) Indiv
Page 13 and 14: Balance of dissipation in the water
Page 15 and 16: Waves and air-sea interactions •
Page 17 and 18: Dependence on breaking Babanin, 201
Page 19 and 20: Wind Input and Wind Stress � �
Page 21 and 22: White Cap Dissipation S ds 2) Indiv
Page 23 and 24: Air-sea interactions at extreme win
Page 25 and 26: Yasi - along-track comparison • d
Page 27 and 28: Babanin, A.V., T.-W. Hsu, A. Roland
Page 29 and 30: Swell attenuation due to wave turbu
Page 31 and 32: Wind/Wave Climate
Page 33 and 34: Wind Trends, by SSM/I
Page 35 and 36: Wind Trends, by SSM/I
Page 37 and 38: ● Numerical Modelling ● Sedimen
Page 39 and 40: ● Numerical Modelling ● Sedimen
Page 41 and 42: Motivation Propagation of waves thr
Page 43 and 44: Young, I.R., Babanin, A.V., Stiassn
Page 45 and 46: Cyclone Wave Modelling • Change o
Page 47 and 48: Shats, M., Babanin, A.V., Marusic,
Page 49 and 50: Air-Sea Gas Exchanges in Extreme Co
Page 51 and 52: Yasi - inner grid • wave height f
Page 53 and 54: Potential role of the wave-induced
Page 55 and 56: Laboratory Experiment at ASIST, RSM
Page 57 and 58:
�K �T s mean �U i CURR �K
Page 59 and 60:
Ghantous et al., Ocean Modelling, s
Page 61 and 62:
Implementing wave-induced mixing in
Page 63 and 64:
Qiao at al., 2010 Globally averaged
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Role of Ocean Waves in the Coupled Atmosphere-Ocean ... - ecmwf

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