The Great Plains low-level jet during the warm season of 1993

• Published in: Monthly weather review Vol. 125; no. 9; pp. 2176 - 2192
• Main Authors: ARRITT, R. W, RINK, T. D, SEGAL, M, TODEY, D. P, CLARK, C. A, MITCHELL, M. J, LABAS, K. M
• Format: Journal Article
• Language: English
• Published: Boston, MA American Meteorological Society 01.09.1997
• Subjects: Earth, ocean, space; Exact sciences and technology; External geophysics; Meteorology; Winds and their effects; Great Plains of America; Mississippi River Basin; North America; America; Great Plains, Central U.S; Climatology; Rain; Ageostrophic wind; Wind field; Geographic distribution; Occurrence frequency; Geostrophic wind; Low level jet; Radar echo
• ISSN: 0027-0644; 1520-0493
• DOI: 10.1175/1520-0493(1997)125<2176:tgpllj>2.0.co;2

Hourly wind profiler observations from the NOAA Profiler Network were used to develop a climatology of the low-level jet (LLJ) over the Great Plains of the central United States from April to September of 1993. The peak precipitation episode of the 1993 flood was associated with a sustained period of high incidence of strong low-level jets (over 20 m s super(-) super(1) ). Consistent with previous studies, strong low-level jets were found to be promoted in the warm sector of an extratropical cyclone. Comparison of datasets formulated using velocity variance thresholds with unthresholded data similar to the operational hourly data suggests that the profiler observations often were contaminated by radar returns from migrating birds, especially during the months of April and May. The strong low-level jets during the peak precipitation episode of the 1993 flood over the upper Mississippi River basin were associated with a high-amplitude upper-level wave pattern over and upstream of the continental United States. Separating the composite 850-mb wind for strong low-level jets into geostrophic and ageostrophic components showed that the magnitudes of the ageostrophic component and the anomalous geostrophic component were comparable.