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Volumn 272, Issue 5269, 1996, Pages 1774-1777

Fine-scale Doppler radar observations of tornadoes

Author keywords

[No Author keywords available]

Indexed keywords

ARTICLE; DISASTER; DOPPLER ECHOGRAPHY; PRIORITY JOURNAL; SHEAR RATE; TELECOMMUNICATION; VELOCITY; WIND;

EID: 0029663009     PISSN: 00368075     EISSN: None     Source Type: Journal    
DOI: 10.1126/science.272.5269.1774     Document Type: Article
Times cited : (116)

References (18)
  • 3
    • 0002979107 scopus 로고
    • E. Kessler, Ed. Univ of Oklahoma Press, Norman, OK, ed. 2
    • R. P. Davies-Jones, in Thunderstorm Morphology and Dynamics, E. Kessler, Ed. (Univ of Oklahoma Press, Norman, OK, ed. 2, 1986), pp. 197-236.
    • (1986) Thunderstorm Morphology and Dynamics , pp. 197-236
    • Davies-Jones, R.P.1
  • 4
    • 0003006113 scopus 로고
    • P. S. Ray, Ed. American Meteorological Society, Boston, MA
    • R Rotunno, in Mesoscale Meteorology and Forecasting, P. S. Ray, Ed. (American Meteorological Society, Boston, MA, 1986), pp. 414-436
    • (1986) Mesoscale Meteorology and Forecasting , pp. 414-436
    • Rotunno, R.1
  • 11
    • 84889509816 scopus 로고    scopus 로고
    • in preparation
    • _, in preparation.
  • 12
    • 84889546352 scopus 로고    scopus 로고
    • note
    • -1 Plotted radar times were 2 min ahead of UTC.
  • 13
    • 84889555763 scopus 로고    scopus 로고
    • note
    • -1, which were manually unfolded to produce the velocity fields shown in the figures
  • 15
    • 84889558791 scopus 로고    scopus 로고
    • note
    • Small-scale suction vortices, 10 to 30 m in diameter, were not unambiguously revealed in either the 50- to 75-m radar resolution volumes of reflectivity or in velocity data retrieved at Dimmitt, TX. It is possible that higher velocities exist in these features, although this was not indicated by the damage survey. Very few structures were struck and therefore damaged by this tornado
  • 16
    • 84889531477 scopus 로고    scopus 로고
    • note
    • We used the following software packages to analyze the data and produce the figures Solo (to display and unfold raw data); Reorder (to interpolate to Cartesian grids); and Zebra (to display gridded data), developed by the Research Data Program of the Atmospheric Technology Division at the National Center for Atmosphere Research (NCAR).
  • 17
    • 84889555677 scopus 로고    scopus 로고
    • note
    • -1 from 185° (from just west of south) was applied to correct for the time skew between low- and high-altitude observations The grid spacing was 50 m. The nearest-neighbor method was used to interpolate to the Cartesian grid
  • 18
    • 84889558129 scopus 로고    scopus 로고
    • note
    • Supported by the University of Oklahoma (J M.S. and J.W.), the National Oceanic and Atmospheric Administration, National Severe Storms Laboratory (NSSL) (E.N R., J.M.S., and J.W.); NCAR, Atmospheric Technology Division, Remote Sensing Facility (J.W.); and the Center for the Analysis and Prediction of Storms through NSF grant ATM-912 0009 (J.M S. and J.W.). The Cooperative Institute for Mesoscale Meteorological Studies, at the University of Oklahoma, also played an important role. The truck for the mobile radar was provided by NSSL (R. Maddox and D Forsythe), and the radar transmitter was provided by NCAR (D. Carlson and P. Hildebrand). M. Randall and E Loew provided the software and hardware for the PC Integrated Radar Acquisition data acquisition system. A. Zahari designed the antenna controller. D. Nealson and P. Griffin provided assistance in building and maintaining the radar L. Chan prepared this manuscript


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