Table 6.2 a Classification of Solid Precipitationa,B,C Typical Forms

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P732951-Ch06.qxd 9/12/05 7:44 PM Page 246 246 Cloud Microphysics Table 6.2 A classification of solid precipitationa,b,c Typical forms Symbol Graphic symbol F1 F2 F3 F4 F5 F6 F7 F8 F9 F10 a Suggested by the International Association of Hydrology’s commission of snow and ice in 1951. [Photograph courtesy of V. Schaefer.] b Additional characteristics: p, broken crystals; r, rime-coated particles not sufficiently coated to be classed as graupel; f, clusters, such as compound snowflakes, composed of several individual snow crystals; w, wet or partly melted particles. c Size of particle is indicated by the general symbol D. The size of a crystal or particle is its greatest extension measured in millimeters. When many particles are involved (e.g., a compound snowflake), it refers to the average size of the individual particles. are required. A more efficient technique might be the seeding, but because neither extensive physical to introduce small water droplets (radius Ӎ30 ␮m) nor rigorous statistical evaluations were carried out, or hygroscopic particles (e.g., NaCl) into the base the results were inconclusive. Recently, there has of a cloud; these particles might then grow by been somewhat of a revival of interest in seeding condensation, and then by collision-coalescence, as warm clouds with hygroscopic nuclei to increase they are carried up and subsequently fall through precipitation but, as yet, the efficacy of this tech- a cloud. nique has not been proven. In the second half of the last century, a number of Seeding with hygroscopic particles has been used cloud seeding experiments on warm clouds were in attempts to improve visibility in warm fogs. carried out using water drops and hygroscopic parti- Because the visibility in a fog is inversely propor- cles. In some cases, rain appeared to be initiated by tional to the number concentration of droplets and.

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