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The radar cross sections of ‘spongy’ ice spheres

✍ Scribed by Battan, Louis J.; Herman, Benjamin M.

Book ID
119724583
Publisher
American Geophysical Union
Year
1962
Tongue
English
Weight
315 KB
Volume
67
Category
Article
ISSN
0148-0227

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## Abstract In supercooled water at temperatures down to‐4·5°C, ice grows in the form of flat dendritic sheets. Between‐4·5° and −5°C a transition in the manner of freezing occurs and three‐dimensional ice structures are produced. At temperatures below‐5·5°C this results in a structure which retain