Bulletin of the American Meteorological Society, Volumen78,Temas9-12American Meteorological Society, 1997 List of members in v. 1, 8. |
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Página 2133
... grid perturbation just men- tioned , the fine - grid perturbation has to be computed to form a total field in the fine - grid RSM . For the first nest- ing , the regional grid value A should be equal to the sum of spherical trans- form ...
... grid perturbation just men- tioned , the fine - grid perturbation has to be computed to form a total field in the fine - grid RSM . For the first nest- ing , the regional grid value A should be equal to the sum of spherical trans- form ...
Página 2134
... grid RSM and to fine - grid RSM becomes simpler . Instead of using several parts to compute the total forc- ing in the regional nesting , the new method needs only the perturbation part from the fine - grid RSM and the base field from ...
... grid RSM and to fine - grid RSM becomes simpler . Instead of using several parts to compute the total forc- ing in the regional nesting , the new method needs only the perturbation part from the fine - grid RSM and the base field from ...
Página 2842
... Grid Boxes 700 600 500 400 300 200 100 2000 0 1850 1900 1950 Year 2000 Figure 2 shows the variation in the number of stations from 1850 to 1997 and the variation in the global cov- erage of the stations as defined by 5 ° × 5 ° grid ...
... Grid Boxes 700 600 500 400 300 200 100 2000 0 1850 1900 1950 Year 2000 Figure 2 shows the variation in the number of stations from 1850 to 1997 and the variation in the global cov- erage of the stations as defined by 5 ° × 5 ° grid ...
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