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Hyodae Seo, Arthur J. Miller, and Joel R. Norris

://gmao.gsfc.nasa.gov/pubs/docs/Chou136.pdf .] Cleveland , W. , 1979 : Robust locally weighted regression and smoothing scatterplots . J. Amer. Stat. Assoc. , 74 , 829 – 836 , doi: 10.1080/01621459.1979.10481038 . Cleveland , W. , and S. J. Devlin , 1988 : Locally weighted regression: An approach to regression analysis by local fitting . J. Amer. Stat. Assoc. , 83 , 596 – 610 . Cornillon , P. , and K.-A. Park , 2001 : Warm core ring velocities inferred from NSCAT . Geophys. Res. Lett. , 28 , 575 – 578 , doi

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

Antarctic Intermediate Water and Labrador Sea Water, the NPIW lacks a corresponding oxygen maximum core and density > 26.8 σ θ does not outcrop in the formation area ( Talley and Nagata 1995 ). Thus, the isopycnal mixing processes between the subarctic and subtropical waters, and the direct ventilation areas, are essential for NPIW formation. From climatological data analysis, Talley (1993) showed that cold and fresh waters are confined to the region between the Kuroshio Extension (KE) and the

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

curl, the fields were therefore estimated from temporally constant coupling coefficients computed separately for each region considered in sections 5 – 6 , with a global (midlatitude) mean coupling coefficient ( Table 2 ). Table 2. Coupling coefficients of surface stress curl perturbation to the crosswind SST gradient anomalies and wind speed perturbation to SST anomalies . For the regional analysis in section 6 , the coupling coefficients are defined to be the regression coefficients

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