. Compendium of meteorology. Meteorology. 518 DYNAMICS OF THE ATMOSPHERE average h or X2 as a function of latitude. They are ob- tained by forming means of h or X2 for groups of sta- tions within fairly small ranges of latitude. For several stations the black dot is "off" the mean curve by more than the length of its uncertainty line. Some such de- partures are to be expected from the laws of chance, but some certainly indicate that L2 does not depend on. plitude is on the whole greatest in the J group of months. Both these features of L2 are illustrated in Fig. 7, for the region of
. Compendium of meteorology. Meteorology. 518 DYNAMICS OF THE ATMOSPHERE average h or X2 as a function of latitude. They are ob- tained by forming means of h or X2 for groups of sta- tions within fairly small ranges of latitude. For several stations the black dot is "off" the mean curve by more than the length of its uncertainty line. Some such de- partures are to be expected from the laws of chance, but some certainly indicate that L2 does not depend on. plitude is on the whole greatest in the J group of months. Both these features of L2 are illustrated in Fig. 7, for the region of North America. Besides the annual mean dial arrow for several United States and Canadian sta- tions, Fig. 7 gives the forward halves of the dial arrows for the J, E, D groups of months. Not every station. 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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