Fig. 1. Weather chart, 13th August, 1912. Typical anticyclone, or “high.” Anticyclone centred North of New Zealand., Fig. 2 is a case where an anticyclone is centred in more northern latitudes, and pressure shows a gradual decrease southwards, in which quarter is the steepest baric gradient. The trend of the isobars is approximately due
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Bibliographic details
New Zealand Journal of Agriculture, Volume XVIII, Issue 6, 20 June 1919, Page 353
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54Fig. 1. Weather chart, 13th August, 1912. Typical anticyclone, or “high.” Anticyclone centred North of New Zealand., Fig. 2 is a case where an anticyclone is centred in more northern latitudes, and pressure shows a gradual decrease southwards, in which quarter is the steepest baric gradient. The trend of the isobars is approximately due New Zealand Journal of Agriculture, Volume XVIII, Issue 6, 20 June 1919, Page 353
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