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Sue Chen, Maria Flatau, Tommy G. Jensen, Toshiaki Shinoda, Jerome Schmidt, Paul May, James Cummings, Ming Liu, Paul E. Ciesielski, Christopher W. Fairall, Ren-Chieh Lien, Dariusz B. Baranowski, Nan-Hsun Chi, Simon de Szoeke, and James Edson

hurricane environment . The mixed layer thickness is calculated based on the depth where the density jump is equivalent to a 3°C temperature change from the 2-m height while holding the salinity constant at the 2-m-level value. These criteria give a shallower MLD but capture the daytime diurnal warm layer and avoid the problem of missing salinity data in the upper 1 m of ocean from the sea glider. Fig . 11. Comparisons of COAMPS (blue) (first and second rows) vertically averaged temperature to 80-m

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