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Hovmöller, Ernest (2011)
Publisher: Co-Action Publishing
Journal: Tellus A
Languages: English
Types: Article
Subjects:
The insufficiency of computed height values for computations of derivatives such as vorticity and convergence, at least for the 300-mb and higher levels, is illustrated by theoretical and practical examples, and it is recommended to make more extensive use of observed winds. This gives a possibility to take into account the cyclostrophic and other non-geostrophic wind components for the vorticity computation which is the first step in the numerical forecasting methods (Charney 1951).DOI: 10.1111/j.2153-3490.1952.tb00996.x
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    • BELLAMJYO, HNC., 1949: Objective Calculations of Divergence, Vertical Velocity and Vorticity. Bull. Am. Met. SOC.30, 2 , pp. 45-49.
    • BYERSH, . R., and RODEBUSHH,. R., 1948: Causes of Thunderstorms of the Florida Peninsula.]. Meteor. 6, pp. 275-280.
    • BYERSH,. R., and HULL,EDWINC., 1949: Inflow Patterns of Thunderstorms as Shown by Winds Aloft. Bdf. Am. Met. Soc, 30, 3 , pp. 90-96.
    • CHARNEJY. ,G., 1951: Dynamic Forecasting by Numerical Process. Compendium of Meteorology, pp. 470- 482.
    • NEWTOCN., W., PHILLIPNS,. A., CARSONJ,. E., and BRADBURYD,. L., 1951: Structure of Shear Lines near the Tropopause in Summer. Tcllus 3, 3, pp. 154-171.
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