Download PDF by H.E. Landsberg (Ed.): Advances in Geophysics, Vol. 2

By H.E. Landsberg (Ed.)

ISBN-10: 0120188023

ISBN-13: 9780120188024

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Extra resources for Advances in Geophysics, Vol. 2

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27. Reflectivity (in decibels) of randomly oriented ice spheroids coated with a confocal film of water, relative to reflectivity of an equivolumic water sphere. Melting ratio, S = (volume of liquid water)/(total volume). ) by catching a sample of snowflakes, melting them, measuring ZD6 for the resulting drops, allowing for the dielectric factor and, of course, for the terminal velocity. As shown in Fig. 25, the effect of the shape of (dry) ice particles on Za is generally unimportant, never as great as a factor of two.

J. Roy. Meteorol. 77, 33-43. 46. Rigby, E. , Marshall, J. , and Hitschfeld, W. (1954). Development during fall of raindrop size distributions, J . Meteorol. 11, 362-372. 47. Bowen, E. G. (1950). The formation of rain by coalescence. Australian J . Scz. Research. 3, 193-213. 48. Reynolds, S. , and Braham, R. (1952). Significance of the initial radar echo. Bull. A m . Meteorol. 33, 123. 49. Braham, R. , Reynolds, S. , and Harrell, J. H. (1951). Possibilities for cloud seeding as determined by a study of cloud height versus precipitation.

Battan, L. J. (1953). Observations on the formation and spread of precipitation in convective clouds. J. Meteorol. 10, 311-324. 42. Workman, E. , and Reynolds, S. E. (1949). Electrical activity as related to thunderstorm cell growth. Bull. A m . Meteorol. 30, 142-144. 43. Jones, R. F. (1950). The temperatures at the top of radar echoes associated with various cloud systems. Quart. J . Roy. Meteorol. Soc. 76, 312-330. 44. Hilst, G. , and MacDowell, G. P. (1950). Radar measurements of the initial growth of thunderstorm precipitation cell8.

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Advances in Geophysics, Vol. 2 by H.E. Landsberg (Ed.)

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