Characteristic Features of Supercooled Raindrops in the Mid-Winter Season of Arctic Canada
Author:
Affiliation:
1. Department of Earth Science, College of Education, Akita University
2. Earth Science Laboratory, Asahikawa College, Hokkaido University of Education
3. Department of Geophysics, Faculty of Science, Hokkaido University
Publisher
Meteorological Society of Japan
Subject
Atmospheric Science
Link
https://www.jstage.jst.go.jp/article/jmsj1965/66/2/66_2_393/_pdf
Reference14 articles.
1. Bocchieri, J.R., 1980: The objective use of upper air sounding to specify precipitation type. Mon. Wea. Rev., 108, 596-603.
2. Joss, J., J.C. Thams and A. Waldvogel, 1968: The variation of raindrop size distributions at Locarno. Proc. In t. Conf Cloud Physics, Toronto. Amer. Meteor. Soc., 369-373.
3. Kajikawa, M. and K. Sakurai, 1987: General description of meteorological conditions and shapes of snow crystals during the observation period at Yellowknife, N.W.T., Canada. Studies on the Snow Crystals of Low Temperature Types and Arctic Aerosols, Hokkaido Univ., Japan, 283pp. (Edited by K. Kikuchi).
4. Kikuchi,.K., 1972: On snow crystals with small raindrops. J. Meteor. Soc. Japan, 50, 142-144.
5. Kikuchi,.K. and H. Uyeda, 1979: Cloud droplets and raindrops collected and frozen on natural snow crystals. J. Meteor. Soc. Japan. 57, 213-281.
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