Variation of temperature in the troposph
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J. K. Bannon; A. Gilchrist
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Article
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1956
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John Wiley and Sons
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English
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## Abstract Correlation coefficients are evaluated between temperatures at 500 mb and at three levels in the lower stratosphere (highest 60 mb) and, respectively, the pressure at the tropopause and the height of the 300โmb level for Larkhill and Lerwick for each month of the year. Similar coefficie