IX.—On some Causes of the Formation of Anticyclonic Stratus as observed from Aeroplanes
1918 ◽
Vol 37
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pp. 137-148
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Keyword(s):
SUMMARYThe following is a summary of the more important conclusions which have been put forward in this paper:—1. The Nature and Distribution of Stratus in Anticyclones.(1) Stratus clouds have an adiabatic temperature gradient below them, and a reversed gradient above them; within the cloud the gradient is usually adiabatic. The same relations hold for well-defined layers of haze.(2) On the northern and eastern sides of anticyclones there is nearly always a layer of stratus, or of haze with cloud patches; the height of this layer varies between 3000 and 6000 feet above the surface, but the level is usually the same over a very large area.(3) Stratus is common in winter on the southern sides of anticyclones.
1971 ◽
Vol 42
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pp. 130-135
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1980 ◽
Vol 27
(1)
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pp. 71-78
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1973 ◽
Vol 20
(4)
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pp. 401-408
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2007 ◽
Vol 168
(2)
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pp. 890-894
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1974 ◽
Vol 64
(2)
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pp. 369-374
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