Urban hailstorms are rarely studied in detail. This work documents five urban storms in Alberta where damage has, on three occasions, set the record for Canada's most costly natural disaster. Information from newspapers, insurance companies, and disaster assistance programs was utilized to supplement meteorological records and information obtained from public surveys.The record-breaking hail swath which accompanied the 1987 Edmonton tornado was mapped using over 800 responses to an unprecedented newspaper survey. Tennis ball sized hail struck 125 km2 of the city. Record-sized hailstones for Alberta were collected. Citizens' measurements of giant hailstones were compared to laboratory measurements. The rural storms were tracked using lightning detector information and damage was mapped using crop insurance and disaster assistance claims. The tornado-bearing storm was found to have a unique track.A late-season hailstorm which struck Calgary in 1991 was mapped using homeowner insurance claims organized by postal areas. Nine out of thirty areas had claims rates exceeding 50%, mainly for shingle replacement. Experiences of claims adjustors and an informal public survey were also utilized. Rural storms were mapped using weather radar and crop losses. The radar beam was strongly attenuated when it passed through hail-bearing storms and, thus, its ability to detect large hail was compromised.Weather conditions, urban and rural damaged areas, and insurance payments were compared for all five local hailstorms. These storms were discussed within the context of the long history of Alberta hail research and current trends in technology implementation. Forecasting of these hailstorms using conventional severe weather indicators was difficult in Calgary because of that city's proximity to the mountains. Hailstorms that struck Munich, Denver, and Toowoomba (Australia) were also discussed, and the hailstones collected from the great Munich storm were compared to those collected from the Edmonton storms.
[1]
Kais J. Al-Jumily,et al.
Identification of Rain and Hail with Circular Polarization Radar
,
1991
.
[2]
R. Wood,et al.
Hail: The White
,
1993
.
[3]
Robert L. Jones,et al.
Canadian disasters: An historical survey
,
1992
.
[4]
Frederick P. Ostby,et al.
Tornadoes of 1990: An all-time Record Year
,
1991
.
[5]
Charles A. Doswell,et al.
Climatology of Nontornadic Severe Thunderstorm Events in the United States
,
1985
.
[6]
D. Roos,et al.
A comparative study of hailstorms in Switzerland, Canada and South Africa
,
1985
.
[7]
N. Balakrishnan,et al.
Estimation of Rain and Hail Rates in Mixed-Phase Precipitation
,
1990
.
[8]
S Leivesley.
Toowoomba: victims and helpers in an Australian hailstorm disaster.
,
1977,
Disasters.
[9]
Narayan R. Gokhale,et al.
Hailstorms and hailstone growth
,
1975
.
[10]
Gerhard A Berz.
List of major natural disasters, 1960–1987
,
1988
.
[11]
Anthony R. Holt,et al.
Separation of Propagation and Backscattering Effects in Rain for Circular Polarization Diversity S-Band Radars
,
1993
.
[12]
Tetsuya Theodore. Fujita,et al.
Tornadoes around the World
,
1973
.
[13]
A. R. Holt,et al.
Radar measurement of rainfall by differential propagation phase: A pilot experiment
,
1991
.
[14]
D. Heimann,et al.
The Munich Hailstorm of July 12, 1984: A Discussion of the Synoptic Situation
,
1985
.
[15]
M. Yau,et al.
The Causes of Severe Convective Outbreaks in Alberta. Part II: Conceptual Model and Statistical Analysis
,
1993
.
[16]
S. Changnon,et al.
Use of Climatological Data in Weather Insurance
,
1990
.