. Compendium of meteorology. Meteorology. 594 MECHANICS OF PRESSURE SYSTEMS Exploring the whole frontal zone for nongeostrophic isentropic motion, we find the conditions for down- gliding limited upwards by the zero isovel, while up- zone is about }io in the upper portion, and it is quasi- vertical near the ground, while an intermediate portion around 700-800 mb tilts only by Kso- The general BIS BISMARCK OMA CBI OMAHA COLUMBIA BRR NASHVILLE. 1000 NOV. 8,1948 1500 Z Fig. 12.—Profile of the warm front of the incipient wave on November 8,1948,1500Z, and part of the 500-mb map for the same time.
. Compendium of meteorology. Meteorology. 594 MECHANICS OF PRESSURE SYSTEMS Exploring the whole frontal zone for nongeostrophic isentropic motion, we find the conditions for down- gliding limited upwards by the zero isovel, while up- zone is about }io in the upper portion, and it is quasi- vertical near the ground, while an intermediate portion around 700-800 mb tilts only by Kso- The general BIS BISMARCK OMA CBI OMAHA COLUMBIA BRR NASHVILLE. 1000 NOV. 8,1948 1500 Z Fig. 12.—Profile of the warm front of the incipient wave on November 8,1948,1500Z, and part of the 500-mb map for the same time. Sample evaluations of 2Q: — dvg/dri below diagram. Upper winds: Half barb 5 m sec"', full barb 10 m sec"'.. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original American Meteorological Society. Committee on the Compendium of Meteorology; Malone, Thomas F. Boston : American Meteorological Society
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