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The formation of atmospheric ice crystals by the freezing of droplets
Author(s) -
Bigg E. K.
Publication year - 1953
Publication title -
quarterly journal of the royal meteorological society
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.744
H-Index - 143
eISSN - 1477-870X
pISSN - 0035-9009
DOI - 10.1002/qj.49707934207
Subject(s) - ice nucleus , supercooling , cirrus , ice crystals , cloud physics , atmospheric sciences , ice formation , clear ice , convection , atmosphere (unit) , cloud chamber , materials science , environmental science , chemistry , meteorology , thermodynamics , geology , physics , arctic ice pack , sea ice , nucleation , cloud computing , antarctic sea ice , computer science , nuclear physics , operating system
Abstract Using the results of laboratory experiments on the supercooling of purified water, the freezing of cloud and raindrops is examined. It is shown that at temperatures lower than about −30°C in cold‐box or expansion‐chamber experiments, the drops freeze in approximately the numbers that would be expected if they were pure water. Those that freeze at temperatures higher than about −20°C seem to be more numerous than would be the case if the drops were pure. An interpretation of the main features of the Findeisen and Schulz expansion‐chamber experiments is found to be possible without appealing to the action of foreign ice‐forming nuclei, although there is a discrepancy between calculation and experiment at temperatures higher than about −20°C. In the atmosphere, formation of cirrus clouds is shown to become possible at temperatures below about −35°C, glaciation in stratiform clouds to become appreciable at temperatures below about −20°C and freezing of raindrops in strongly convective clouds to become important below about −13°C, without the presence of ice nuclei. It is concluded that freezing nuclei may be important at temperatures above about −20°C, while their presence at lower temperatures will be masked by the freezing of uncontaminated drops.