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

of potential severe convective environments across South Africa . Climate Dyn. , 49 , 2161 – 2178 , https://doi.org/10.1007/s00382-016-3434-7 . 10.1007/s00382-016-3434-7 Camilloni , I. A. , and V. R. Barros , 2003 : Extreme discharge events in the Parana River and their climate forcing . J. Hydrol. , 278 , 94 – 106 , https://doi.org/10.1016/S0022-1694(03)00133-1 . 10.1016/S0022-1694(03)00133-1 Cavalcanti , I. F. A. , and Coauthors , 2015 : Precipitation extremes over La Plata

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