| Publication Date |
1978 |
| Personal Author |
Fujita, T. T. |
| Page Count |
118 |
| Abstract |
The evidence of downbursts available as of this date are presented. Straight-line winds, often preceded by an awesome-looking roll cloud, can induce widespread wind damage in and around thunderstorm areas. Extensive aerial photography and mapping of the areas swept by straight-line winds has revealed the existence of diverging patterns of damage embedded inside of overall straight-line flows. A major breakthrough in this study was the analysis of the Independence Day, 1977 storms in Northern Wisconsin. At least 25 locations of divergent downburst flow were mapped from a low-flying aircraft. Microscale downbursts (microbursts), less than 3 miles in outflow diameter, were found in other parts of the country. Four aircraft accidents in 1975-77 and one more in 1956 have been related to microbursts whose sizes were comparable to the length of runways. Damaging winds of a microburst last only for a few minutes. Downburst damage is often highly localized, resembling that of tornadoes. Insight into operational applications of these findings are presented. These assessments should be useful in ascertaining whether or not storm damage is tornado or downburst related. |
| Keywords |
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| Source Agency |
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| NTIS Subject Category |
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| Corporate Authors |
Chicago Univ., Ill. Dept. of the Geophysical Sciences.; National Aeronautics and Space Administration, Washington, D.C.; National Weather Service, Silver Spring, MD.; Nuclear Regulatory Commission, Washington, D.C. |
| Supplemental Notes |
Sponsored in part by National Aeronautics and Space Administration, Washington, D.C. Grant NGR-14-001-008. Report on Satellite and Mesometeorology Research Project. |
| Document Type |
Technical Report |
| Title Note |
Research paper. |
| NTIS Issue Number |
197825 |
| Contract Number |
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