By A. J. Chisholm, Marianne English (auth.)
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Extra resources for Alberta Hailstorms
AI though it has been assumed that these embryos exist throughout the WER, this is not necessary to produce large hail. They could, for instance, be found just around the edges of the WER and not in the middle. The embryos travel through the storm as indicated in Fig. 1, growing by colliding with and collecting supercooled cloud droplets. In regions where radar FrG. 2. Photogra ph of thin section of a hailstone collected from the hailstorm that occurred over Montreal Isla nd on 1 August 1969. 03 em, respectively .
Lines AB and CD indicate cross-section axes for Figs. 40 and 41. 30 :VIETEOROLOGICAL MONOGRAPHS WIND -20 COMPONENT -10 RELATIVE 0 +10 •20 TO +30 STORM VoL. 14, No. ~,-,--,-,-,~,-,-,--,-, 29 JUNE 1967 4 6 10 12 HORIZONTAL 14 DISTANCE 16 (km) 18 20 22 24 26 FIG. 40. Schematic airflow in the plane of storm motion, 29 June 1967. The inflow air enters on the downwind side of the storm, tilting upwind while ascending through the B\VER. Under the influence of strong relative winds above 5 km, the updraft tilts rapidly downstream, reaching the storm top downwind from its point of entry.
Appl. , 5, 461-466. ~-,and J. D. Marwitz, 1968: Estimates of air and moisture flux into hailstorms on the high plains. J. Appl. , 7, 196-198. Bates, F. , and C. \V. Newton, 1965: The forms of updrafts and downdrafts in cumulonimbus in a sheared environment. Paper presented at Amer. Meteor. Soc. meeting on Cloud Physics and Severe Local Storms, Reno, Nev. (mimeographed, 9 pp plus figures). Browning, K. , 1965: A family outbreak of severe local stormsA comprehensive study of the storms in Oklahoma on 26 May 1963.
Alberta Hailstorms by A. J. Chisholm, Marianne English (auth.)