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Atlantic Meridional Transport Observed From Space Preliminry Results W. Timothy Liu and Xiaosu Xie Heat Transport Water Transport Mean and Seasonal Variation
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Center of cyclonic currents Ekman water transport Ekman heat transport τ x : Zonal stress Te: Potential temp. of Ekman layer : Mean potential temp. of the water column Sato, Polito, & Liu, 2002: GRL, 29(17) Sprintall & Liu, 2005: Oceanography, 18(4)
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Center of cyclonic currents Meridional Heat Transport (MHT) H: Heat content ζ: Horizontal heat flux SW: Short wave radiation LW: Long wave radiation LH: Latent heat SH: Sensible heat By Green’s theorem Conservation of heat
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Center of cyclonic currents Meridional Water Transport (MWT) P: Precipitation E: Evaporation Ψ: Horizontal mass flux R: River discharge By Green’s theorem Conservation of water mass
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Total MHT at Atlantic MHT from surface heat flux MHT from heat storage change (Statistic- al model)
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Intensification of poleward Ekman water transport from 1998 in the tropics Pacific Ekman water transport Anomaly Total
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Intensification of poleward Ekman heat transport from 1999 in the tropical Atlantic Ekman heat transport anomaly 12N-14N SSM/I QuikSCAT 5S-8S
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Ekman water transport in the subtropical Atlantic is correlated with NAO
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Atlantic total northward water transport Atlantic Ekman water transport Peak poleward transport in winter in the tropics
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Intensification of poleward Ekman water transport from 1998 in the tropics Atlantic Ekman water transport Total Anomaly
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Ekman water transport anomaly 12N-14N SSM/I QuikSCAT 5S-8S Intensification of poleward Ekman water transport from 1998 in the tropical Atlantic
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Ekman water transport in the subtropical Atlantic is correlated with NAO
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Summary Spacebased data provide almost continuous spatial and temporal coverages for Ekman and total meridional transport for a decade Reality checks are needed What is the relation between surface Ekman transport in the total meridional transport need physical interpolation.
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