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The Global ETD Search service is a free service for researchers
to find electronic theses and dissertations. This service is
provided by the
Networked Digital Library of Theses and Dissertations.
Our metadata is collected from universities around the world. If you manage a university/consortium/country archive and want to be added, details can be found on the NDLTD website.
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Showing 1 to 8 of 8 (0.046 seconds)Spelling suggestions: "subject:"fail -- alberta."" "subject:"fail -- elberta.""
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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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A radar study of seeded Alberta hailstorms /Inkster, Don Robert January 1977 (has links)
No description available.
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| 3 |
The continuity of hail production in Alberta storms.Williams, Geoffrey Neville. January 1963 (has links)
A study was made in Alberta of the pattern of hailfall from four swath-giving storms, in order to determine whether or not, within the borders of the swath, there existed local hail-free regions. [...]
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| 4 |
The continuity of hail production in Alberta storms.Williams, Geoffrey Neville. January 1963 (has links)
No description available.
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| 5 |
Small scale radar structure of Alberta hailstorms.Chisholm, Alexander James January 1966 (has links)
A radar study of two Alberta hailstorms has revealed the existence of small cellular radar echoes with durations of 10-30 minutes. These cells were found to group together to form storm families which existed for several hours. New cells invariably formed on the southern end of the storm family and migrated northward through the storm to dissipate on the northern boundary. [...]
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| 6 |
Small scale radar structure of Alberta hailstorms.Chisholm, Alexander James January 1966 (has links)
No description available.
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| 7 |
The influence of wind shear on Alberta hail storm activity.Proppe, Harold W. (Harold Walter). January 1965 (has links)
Vertical wind shear is computed between the 28 possible pairs of the first 8 mandatory radiosonde levels. A hail severity index is defined. Statistically significant correlations between strong shear and hail-free days are found in 11 shear layers. Strong shears are also found to occur more frequently with low and high severity indices than with intermediate severity indices. [...]
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| 8 |
The influence of wind shear on Alberta hail storm activity.Proppe, Harold W. (Harold Walter). January 1965 (has links)
No description available.
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