Bulletin of the American Meteorological Society, Volumen49American Meteorological Society, 1968 Vols. for 1990- contain supplemental membership directory. |
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Página 347
... crystals is shown in the upper part of Fig . 5. The solid line was derived by combining observations on the relative rate of growth of ice crystals as reported by Hallett ( 1965 ) with laboratory measurements of actual growth rates of ...
... crystals is shown in the upper part of Fig . 5. The solid line was derived by combining observations on the relative rate of growth of ice crystals as reported by Hallett ( 1965 ) with laboratory measurements of actual growth rates of ...
Página 350
... crystals could survive - how far cirrus crystals could fall - in clear air before com- plete evaporation . Much of this uncertainty was re- moved by recent studies of The University of Chicago Group ( Braham , 1967 ; Braham and Spyers ...
... crystals could survive - how far cirrus crystals could fall - in clear air before com- plete evaporation . Much of this uncertainty was re- moved by recent studies of The University of Chicago Group ( Braham , 1967 ; Braham and Spyers ...
Página 601
... crystal shapes and of the center part of snow crystals . 3 ) The aggregation phenomena of ice crystals . 4 ) Irregular snow crystals in colder temperature regions . 5 ) The riming phenomena of supercooled cloud droplets on snow crystals ...
... crystal shapes and of the center part of snow crystals . 3 ) The aggregation phenomena of ice crystals . 4 ) Irregular snow crystals in colder temperature regions . 5 ) The riming phenomena of supercooled cloud droplets on snow crystals ...
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