Bulletin of the American Meteorological Society, Volumen49American Meteorological Society, 1968 Vols. for 1990- contain supplemental membership directory. |
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Página 134
... layer flow at these distances . A momentum integral method is used to follow the boundary layer develop- ment to the center regions of the vortex . Radial profiles of boundary layer thickness and induced vertical velocity are obtained ...
... layer flow at these distances . A momentum integral method is used to follow the boundary layer develop- ment to the center regions of the vortex . Radial profiles of boundary layer thickness and induced vertical velocity are obtained ...
Página 251
... layer All methods discussed so - far require non - routine mea- surements and very specialized efforts . In many cases , the rationale for their use is the hope that reliable stress determinations , obtained under a sufficiently wide ...
... layer All methods discussed so - far require non - routine mea- surements and very specialized efforts . In many cases , the rationale for their use is the hope that reliable stress determinations , obtained under a sufficiently wide ...
Página 355
... layer at the surface . The great overall stability holds the moisture near the surface . When the east winds die down and the normal north - westerly regime begins , fog is created in the thin surface layer at sea as the warm , nearly ...
... layer at the surface . The great overall stability holds the moisture near the surface . When the east winds die down and the normal north - westerly regime begins , fog is created in the thin surface layer at sea as the warm , nearly ...
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