Bulletin of the American Meteorological Society, Volumen48American Meteorological Society, 1967 Vols. for 1990- contain supplemental membership directory. |
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Página 535
... pressure • In the equation for the lowest stratum the corresponding term - m , does not appear FIG . 7. Computing Form P XIII . ( Reproduction of p . 200 of the book . CGS units are used throughout . ) This is the fateful form on which ...
... pressure • In the equation for the lowest stratum the corresponding term - m , does not appear FIG . 7. Computing Form P XIII . ( Reproduction of p . 200 of the book . CGS units are used throughout . ) This is the fateful form on which ...
Página 619
... pressure of a tropical storm when an eye is seen by satellites is found to vary between 945 and 970 mb . The wind and pressure fields relative to the storm center have been studied on the basis of storms which occurred in the Indian ...
... pressure of a tropical storm when an eye is seen by satellites is found to vary between 945 and 970 mb . The wind and pressure fields relative to the storm center have been studied on the basis of storms which occurred in the Indian ...
Página 837
... pressure deviation is zero all along the upper boundary in the first case , or that the pressure deviation is zero at the upper left corner grid point in the second case , with the addi- tional boundary values obtained from the first ...
... pressure deviation is zero all along the upper boundary in the first case , or that the pressure deviation is zero at the upper left corner grid point in the second case , with the addi- tional boundary values obtained from the first ...
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