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- W2170643208 abstract "A database consisting of approximately 4000 storm observations has been objectively analyzed to determine environmental characteristics that produce high radar reflectivities above the freezing level, large total lightning flash rates on the order of 10 flashes per minute, and anomalous vertical charge structures (most notably, dominant midlevel positive charge). The storm database is drawn from four regions of the United States featuring distinct environments, each with coinciding Lightning Mapping Array (LMA) network data. LMAs are able to infer total lightning flash rates using flash clustering algorithms, such as the one implemented in this study. Results show that anomalous charge structures inferred from LMA data, significant lightning flash rates, and increased radar reflectivities above the freezing level tend to be associated with environments that have high cloud base heights (approximately 3 km above ground level) and large atmospheric instability, quantified by normalized convective available potential energy (NCAPE) near 0.2 m s−2. Additionally, we infer that aerosols may affect storm intensity. Maximum flash rates were observed in storms with attributed aerosol concentrations near 1000 cm−3, while total flash rates decrease when aerosol concentrations exceed 1500 cm−3, consistent with previous studies. However, this effect is more pronounced in regions where the NCAPE and cloud base height are low. The dearth of storms with estimated aerosol concentrations less than 700 cm−3 (approximately 1% of total sample) does not provide a complete depiction of aerosol invigoration." @default.
- W2170643208 created "2016-06-24" @default.
- W2170643208 creator A5012079319 @default.
- W2170643208 creator A5033983693 @default.
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- W2170643208 creator A5087393269 @default.
- W2170643208 creator A5090863264 @default.
- W2170643208 date "2015-07-07" @default.
- W2170643208 modified "2023-10-06" @default.
- W2170643208 title "Environmental controls on storm intensity and charge structure in multiple regions of the continental United States" @default.
- W2170643208 cites W1508776603 @default.
- W2170643208 cites W1653983574 @default.
- W2170643208 cites W1965510025 @default.
- W2170643208 cites W1965595694 @default.
- W2170643208 cites W1968136240 @default.
- W2170643208 cites W1969005344 @default.
- W2170643208 cites W1970588407 @default.
- W2170643208 cites W1973218717 @default.
- W2170643208 cites W1974584236 @default.
- W2170643208 cites W1976126293 @default.
- W2170643208 cites W1977701038 @default.
- W2170643208 cites W1979959032 @default.
- W2170643208 cites W1981558409 @default.
- W2170643208 cites W1983299260 @default.
- W2170643208 cites W1987324508 @default.
- W2170643208 cites W1988160716 @default.
- W2170643208 cites W1995415131 @default.
- W2170643208 cites W1997344618 @default.
- W2170643208 cites W1998349300 @default.
- W2170643208 cites W1998652360 @default.
- W2170643208 cites W2000756850 @default.
- W2170643208 cites W2002898709 @default.
- W2170643208 cites W2005552249 @default.
- W2170643208 cites W2006110206 @default.
- W2170643208 cites W2007427110 @default.
- W2170643208 cites W2009031048 @default.
- W2170643208 cites W2009227399 @default.
- W2170643208 cites W2010292247 @default.
- W2170643208 cites W2010398575 @default.
- W2170643208 cites W2013805876 @default.
- W2170643208 cites W2016184960 @default.
- W2170643208 cites W2020712283 @default.
- W2170643208 cites W2021002860 @default.
- W2170643208 cites W2022357051 @default.
- W2170643208 cites W2022474024 @default.
- W2170643208 cites W2025358446 @default.
- W2170643208 cites W2028797398 @default.
- W2170643208 cites W2030464877 @default.
- W2170643208 cites W2031675844 @default.
- W2170643208 cites W2033229218 @default.
- W2170643208 cites W2033455002 @default.
- W2170643208 cites W2035161396 @default.
- W2170643208 cites W2035769711 @default.
- W2170643208 cites W2036379407 @default.
- W2170643208 cites W2036514338 @default.
- W2170643208 cites W2039169660 @default.
- W2170643208 cites W2039848571 @default.
- W2170643208 cites W2042361863 @default.
- W2170643208 cites W2046805998 @default.
- W2170643208 cites W2051439870 @default.
- W2170643208 cites W2058334289 @default.
- W2170643208 cites W2065626194 @default.
- W2170643208 cites W2066661515 @default.
- W2170643208 cites W2070381285 @default.
- W2170643208 cites W2070787619 @default.
- W2170643208 cites W2071887418 @default.
- W2170643208 cites W2074230297 @default.
- W2170643208 cites W2077301893 @default.
- W2170643208 cites W2081618373 @default.
- W2170643208 cites W2081930613 @default.
- W2170643208 cites W2081987809 @default.
- W2170643208 cites W2082822241 @default.
- W2170643208 cites W2083128385 @default.
- W2170643208 cites W2085149507 @default.
- W2170643208 cites W2086827868 @default.
- W2170643208 cites W2089433206 @default.
- W2170643208 cites W2095722067 @default.
- W2170643208 cites W2100234364 @default.
- W2170643208 cites W2101947122 @default.
- W2170643208 cites W2102641689 @default.
- W2170643208 cites W2106123550 @default.
- W2170643208 cites W2109345045 @default.
- W2170643208 cites W2109541362 @default.
- W2170643208 cites W2109839958 @default.
- W2170643208 cites W2109984465 @default.
- W2170643208 cites W2110565131 @default.
- W2170643208 cites W2110899229 @default.
- W2170643208 cites W2111787820 @default.
- W2170643208 cites W2111876452 @default.
- W2170643208 cites W2115334653 @default.
- W2170643208 cites W2122360723 @default.
- W2170643208 cites W2128668343 @default.
- W2170643208 cites W2130662209 @default.
- W2170643208 cites W2131760093 @default.