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Zachary S. Bruick, Kristen L. Rasmussen, Angela K. Rowe, and Lynn A. McMurdie

show why this region is highly favored for convective initiation and subsequent upscale growth. Convergence is maximized near the SDC due to the impingement of the South American low-level jet (SALLJ) from the north and ageostrophic midlevel flow from the south on the elevated terrain. Because of the descent of upper-level air in the lee of the Andes, a mechanical capping inversion exists over the region that inhibits convective initiation. Moisture is advected into subtropical South America from

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Zachary S. Bruick, Kristen L. Rasmussen, and Daniel J. Cecil

1. Introduction Hail in subtropical South America can be very large ( Rasmussen et al. 2014 ) and frequent (10–30 storms per year in central Argentina; Cecil and Blankenship 2012 ), and it causes significant impacts to property and the agricultural economy in this region. Hail has been studied for more than five decades, yet relatively little is known about the storms that produce hail or the environments that support hail-producing storms in subtropical South America. Hail research in the

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Jake P. Mulholland, Stephen W. Nesbitt, Robert J. Trapp, Kristen L. Rasmussen, and Paola V. Salio

.1175/JAMC-D-14-0114.1 . 10.1175/JAMC-D-14-0114.1 Ribeiro , B. Z. , and L. F. Bosart , 2018 : Elevated mixed layers and associated severe thunderstorm environments in South and North America . Mon. Wea. Rev. , 146 , 3 – 28 , . 10.1175/MWR-D-17-0121.1 Romatschke , U. , and R. A. Houze Jr. , 2010 : Extreme summer convection in South America . J. Climate , 23 , 3761 – 3791 , . 10.1175/2010JCLI3465.1 Salio

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Robert J. Trapp, Karen A. Kosiba, James N. Marquis, Matthew R. Kumjian, Stephen W. Nesbitt, Joshua Wurman, Paola Salio, Maxwell A. Grover, Paul Robinson, and Deanna A. Hence

1. Introduction Satellite observations suggest that thunderstorms in southeast South America are among the most intense and deepest in the world ( Zipser et al. 2006 ), are prolific hail producers ( Cecil and Blankenship 2012 ; Mezher et al. 2012 ; Bang and Cecil 2019 ; Bruick et al. 2019 ), and often are accompanied by extreme lightning activity and flooding (e.g., Rasmussen et al. 2014 ). In Argentina specifically, thunderstorm-generated hazards adversely impact a largely urban population

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Hernán Bechis, Paola Salio, and Juan José Ruiz

dryline is required. Some studies ( Owen 1966 ; Hoch and Markowski 2005 ; Schultz et al. 2007 ) use surface observations to manually detect drylines. Based on this approach they found that drylines are observed over the U.S. Great Plains on 32%–45% of the spring season days (April, May, and June). Duell and Van Den Broeke (2016) developed an objective algorithm to detect drylines in the Mississippi River valley (United States), where drylines are less frequent, using data from the North American

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Jake P. Mulholland, Stephen W. Nesbitt, and Robert J. Trapp

initially favor supercells as the primary convective mode, may later favor a more rapid upscale transition into MCSs via cold pool amalgamation and/or surging outflows (e.g., Coniglio et al. 2010 ; Peters et al. 2017 ; and references therein). One region of the world that is susceptible to rapid upscale growth of deep moist convection is the northern half of Argentina, South America. The present study is focused along an approximately north–south mountain chain called the Sierras de Córdoba (SDC) (e

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James N. Marquis, Adam C. Varble, Paul Robinson, T. Connor Nelson, and Katja Friedrich

exceed 35 dB Z for more than 15 min, and thus remains below thresholds utilized by a companion study ( Nelson et al. 2021 ) to classify sustained CI processes. Longer-lived deep convection initiates approximately 60 km north of this cell, outside of the instrument array. Our third case occurred during the PECAN field experiment, which focused on understanding nocturnal CI over the U.S. central plains ( Weckwerth et al. 2019 ). During the evening of 3 July 2015, an informal CI mission was conducted

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