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Synoptic influences on the evolution of a severe hailstorm environmentDuker, Dick C. 23 August 1977 (has links)
Two summertime days were investigated, 27 and 28 June 1973,
to observe the changes in the environment that led to the severe hailstorm
on 28 June in the National Hail Research Experiment (NHRE)
network, Colorado. Within the network thermodynamic analyses
revealed the 28th to have:
(1) Above-average low-level moisture.
(2) Approximately equal heating as on the 27th.
(3) A lower stability index in the morning than on the previous
morning.
(4) A potentially unstable layer at the top of the mixed layer.
The small scale and weakness of an eastward-migrating short
wave trough suggested application of a perturbation wind analysis,
which showed a vortex moving across the country. Divergence computations
at upper levels displayed a divergent region downstream of the
vortex and convergent region upstream. The ascent associated with
this upper-level divergence led to release of the potential instability
found on the 28th, resulting in severe convective storms within the
NHRE network.
Satellite photographs suggest that the short wave trough originated
off the Baja California coast, and show the perturbation vortex associated
clouds to move across the U.S. in good agreement with
estimated locations of the divergence maximum. / Graduation date: 1978
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The structure and motion of some severe hailstorms.Marwitz, John January 1971 (has links)
No description available.
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Hailstone flux through the level of maximum updrift.Donnelly, Arthur M. January 1967 (has links)
No description available.
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The growth of large hail : studies derived from Alberta and Montreal hailstorms.English, Marianne January 1972 (has links)
No description available.
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Hailstone flux through the level of maximum updrift.Donnelly, Arthur M. January 1967 (has links)
No description available.
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The growth of large hail : studies derived from Alberta and Montreal hailstorms.English, Marianne January 1972 (has links)
No description available.
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The structure and motion of some severe hailstorms.Marwitz, John January 1971 (has links)
No description available.
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Small-scale structure of hail swaths.McBride, John Harold. January 1964 (has links)
A study was made of the 3163 replies to the question of continuity during hailfall on all hail reports obtained from non-trained voluntary observers and by personal surveys during the 1963 hail season in Central Alberta, in order to determine the nature of hailstorms. The hailswath of the July 14 major storm featured very large hail in two small areas, and regions of rain-but-no-hail embedded within the swath. The largest hail was related to several small and intense radar echoes, during the first 22 minutes of their existence. Data indicate that Alberta hailstorms appear more or less continuous when studied on a coarse scale; however, when data are available on a finer scale, intermittency becomes evident, which points to the conclusion that hailstorms are composed of a number of small, individual, hail-producing cells acting together within storms. [...]
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A radar study of seeded Alberta hailstorms /Inkster, Don Robert. January 1977 (has links)
No description available.
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Geschichte der hagelversicherung im grossherzogtum Baden ...Weis, Gustav, January 1905 (has links)
Inaug.-diss.--Heidelberg. / Lebenslauf.
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