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pro vyhledávání: '"N. E. J. Boston"'
Publikováno v:
Journal of Geophysical Research. 70:3867-3878
Bathythermographic and wind speed data collected at Ocean Weather Station P (50°N, 145°W) during April through August of the four years, 1956 through 1959, have been examined for relationships between the depth of the isothermal surface layer and t