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Peter Gaube, Dudley B. Chelton, Roger M. Samelson, Michael G. Schlax, and Larry W. O’Neill

.2008.02.005 . Leetmaa , A. , and A. F. Bunker , 1978 : Updated charts of the mean annual wind stress, convergences in the Ekman layers, and Sverdrup transports in the North Atlantic . J. Mar. Res. , 36 , 311 – 322 . Liu , W. T. , and W. Tang , 1996 : Equivalent neutral wind. National Aeronautics and Space Administration/Jet Propulsion Laboratory/California Institute of Technology JPL Publ. 96-17, 22 pp. [Available online at

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Takuya Nakanowatari, Humio Mitsudera, Tatsuo Motoi, Ichiro Ishikawa, Kay I. Ohshima, and Masaaki Wakatsuchi

(northerly) flow over the eastern (western) North Pacific; opposite conditions are obtained for positive values. 3. Climatological features of the model simulation In this section, we assess both the representation of the intermediate water circulation and the water properties in the model simulation by comparing climatological data with those of observations. The model representation of NPIW is also shown in Ishikawa and Ishizaki (2009) , but we here focus on the representation of the frontal and jet

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