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ChuanLi Jiang, Sarah T. Gille, Janet Sprintall, Kei Yoshimura, and Masao Kanamitsu

paucity of in situ observations in the Southern Ocean leaves open a host of questions about the true nature of surface fluxes at high latitudes, and our objectives are to address some of these most basic unknown aspects of Southern Ocean air–sea fluxes. We focus specifically on the turbulent fluxes of sensible and latent heat, which depend strongly on air–sea temperature differences and on specific humidity. In our analysis, we make use of year-round high-resolution shipboard measurements of the flux

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Lei Shi, Ge Peng, and John J. Bates

further improved through refinements to the regression formula, training dataset, collocation procedure, and height adjustment to 10 m ( Jackson et al. 2009 ). Zong et al. (2007) used the Advanced Microwave Scanning Radiometer for Earth Observing System (EOS) (AMSR-E) to derive near-surface specific humidity. Roberts et al. (2010) developed retrieval algorithms based on the neural network technique to derive sea surface temperature, air temperature, specific humidity, and wind speed. Jackson and

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