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- W2109121519 abstract "Abstract On 14–15 February 1992 a long-lived mesoscale gravity wave was observed over the Storm-scale Operational and Research Meteorology-Fronts Experiment Systems Test observational network. A precipitation band formed and intensified as the wave moved across Kansas and Missouri. The disturbance was tracked for 14 h. Surface, dual-Doppler radar, and wind profiler analyses, as well as isentropic analyses derived from a special rawinsonde network, are used to examine the origin and evolution of this wave. The wave originated at the leading edge of a dry air mass associated with downslope flow in the lee of the Rockies. The earliest surface pressure signatures of wave motion began as a dry air mass, associated with the downslope flow, ascended a warm front east of a lee cyclone. A weak rainband developed simultaneously with the wave at the leading edge of the dry air mass. The mesoscale gravity wave, and convection, remained tied to the leading edge of the advancing dry air mass during the first 8–10 h of ..." @default.
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- W2109121519 date "2001-02-01" @default.
- W2109121519 modified "2023-09-28" @default.
- W2109121519 title "Origin, Evolution, and Finescale Structure of the St. Valentine’s Day Mesoscale Gravity Wave Observed during STORM-FEST. Part I: Origin and Evolution" @default.
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- W2109121519 doi "https://doi.org/10.1175/1520-0493(2001)129<0198:oeafso>2.0.co;2" @default.
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