Bulletin of the American Meteorological Society, Volumen82American Meteorological Society., 2001 List of members in v. 1, 8. |
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Página 2236
... layer . On 18-19 July , for example , the upper layer is well mixed in temperature and salinity and about 60 m deep ( Fig . 13b ) . However , on other days , such as 27 August , salin- ity effects can be seen clearly ( Fig . 13c ) ...
... layer . On 18-19 July , for example , the upper layer is well mixed in temperature and salinity and about 60 m deep ( Fig . 13b ) . However , on other days , such as 27 August , salin- ity effects can be seen clearly ( Fig . 13c ) ...
Página 2238
... layer . This halocline is very tight during the first half of the observation period but broadens afterward , indicat- ing the weakening salinity effects on the upper layer . There appears to be an increase in the depth of the halocline ...
... layer . This halocline is very tight during the first half of the observation period but broadens afterward , indicat- ing the weakening salinity effects on the upper layer . There appears to be an increase in the depth of the halocline ...
Página 2841
... layer observations . Radio Sci . , 32 , 1279–1296 . Dalaudier , F. , C. Sidi , M. Crochet , and J. Vernin , 1994 : Direct evidence of " sheets " in the atmospheric temperature field . J. Atmos . Sci . , 51 , 237-248 . Davis , A. B. , A ...
... layer observations . Radio Sci . , 32 , 1279–1296 . Dalaudier , F. , C. Sidi , M. Crochet , and J. Vernin , 1994 : Direct evidence of " sheets " in the atmospheric temperature field . J. Atmos . Sci . , 51 , 237-248 . Davis , A. B. , A ...
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