. Compendium of meteorology. Meteorology. Fig. 6.—Contours of the SOO-mb surface (in tens of dynamic meters) for January 11, 1949 at 0200 GMT. Example of a cir- cumpolar zonal circulation. unusual path. This is also an example of the fact that relatively warm anticyclones in the upper troposphere can occur at rather high latitudes even during the. Fig. 6.^Contours of the 500-mb surface (in tens of dy- namic meters) for June 23, 1949 at 0200 GMT. Example of a circulation in the form of elongated meridional circulation cells (Zirkulationsstreifen). winter season. (Regarding zonal displacements o
. Compendium of meteorology. Meteorology. Fig. 6.—Contours of the SOO-mb surface (in tens of dynamic meters) for January 11, 1949 at 0200 GMT. Example of a cir- cumpolar zonal circulation. unusual path. This is also an example of the fact that relatively warm anticyclones in the upper troposphere can occur at rather high latitudes even during the. Fig. 6.^Contours of the 500-mb surface (in tens of dy- namic meters) for June 23, 1949 at 0200 GMT. Example of a circulation in the form of elongated meridional circulation cells (Zirkulationsstreifen). winter season. (Regarding zonal displacements of wedges and troughs, see p. 830.) The centers of high- and low-pressure cells at the 5-km level for the period from June 21 to July 5, 1949 are shown in Fig. 7. In each of the regions marked I and III there is a moving low-pressure center (the one of region III splits at times). Regions II and IV each con- tain a high-pressure center and show, in particular, the small zonal displacement. On June 27 and 28, a stronger zonal movement occurred, to the northeast for region. 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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