2015
DOI: 10.15191/nwajom.2015.0313
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Warm-season thunderstorm development as a function of vertical distribution of relative humidity in the Lower Rio Grande Valley of Texas

Abstract: Weakly forced large-scale weather patterns often dominate the warm season (June-September) in the Lower Rio Grande Valley of Texas. In this regime, forecasting thunderstorm development is often tied to very subtle features, making this task particularly challenging. There appears to be a link between middleand lower-level moisture content (specifically at 850-700 hPa) and the frequency of thunderstorm development, with little variability in many other meteorological variables. Higher 850-700-hPa relative humid… Show more

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Cited by 1 publication
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“…High RH of about is found upto 400 hPa. High values of RH (moisture) between low and mid troposphere increase the probability of occurrence of thunderstorm 23 .…”
Section: K-index(ki) and Total Totals Index (Tti)mentioning
confidence: 99%
“…High RH of about is found upto 400 hPa. High values of RH (moisture) between low and mid troposphere increase the probability of occurrence of thunderstorm 23 .…”
Section: K-index(ki) and Total Totals Index (Tti)mentioning
confidence: 99%