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Variation with height of rainfall below the melting level

✍ Scribed by W. G. Harper

Publisher
John Wiley and Sons
Year
1957
Tongue
English
Weight
321 KB
Volume
83
Category
Article
ISSN
0035-9009

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✦ Synopsis

Abstract

3‐cm radar signal intensity measurements, made at a range of heights up to 6,000 ft on three days with widespread moderate rain, suggest that there was considerable uniformity of drop‐size distribution and of rainfall rate with height once melting of snowflakes was complete and terminal velocity was achieved, and that in these warm‐front type situations no significant growth of precipitation was taking place below the melting layer.

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