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Youichi Tanimoto, Kou Shimoyama, and Shoichi Mori

1. Introduction Continuous and repeated in situ observations of the marine atmospheric boundary layer (MABL) along specific cross sections are very scarce over coastal regions and even rarer over the open oceans. Several previous studies, however, have conducted shipboard atmospheric soundings along a single cross section using a global positioning system (GPS) sonde. These studies have been successful in showing the distinct transition of temperature and moisture in the MABL across the steep

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