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. Soc. , 122 , 73 – 119 , doi: 10.1002/qj.49712252905 . Morss, R. E. , Lazo J. K. , Brown B. G. , Brooks H. E. , Ganderton P. T. , and Mills B. N. , 2008 : Societal and economic research and applications for weather forecasts: Priorities for the North American THORPEX program . Bull. Amer. Meteor. Soc. , 89 , 335 – 346 , doi: 10.1175/BAMS-89-3-335 . Neu, U. , and Coauthors , 2013 : IMILAST: A community effort to intercompare extratropical cyclone detection and tracking
. Soc. , 122 , 73 – 119 , doi: 10.1002/qj.49712252905 . Morss, R. E. , Lazo J. K. , Brown B. G. , Brooks H. E. , Ganderton P. T. , and Mills B. N. , 2008 : Societal and economic research and applications for weather forecasts: Priorities for the North American THORPEX program . Bull. Amer. Meteor. Soc. , 89 , 335 – 346 , doi: 10.1175/BAMS-89-3-335 . Neu, U. , and Coauthors , 2013 : IMILAST: A community effort to intercompare extratropical cyclone detection and tracking
region. The term refers to Grønås's (1995) invocation of the “poisonous tail of the bent-back occlusion,” deriving from the Norwegian School's recognition of strong winds at the end of a bent-back occluded front in many cyclones that are now known as Shapiro–Keyser (1990) cyclones. Wind speed maxima resembling sting jets have been identified in other North Atlantic, North Pacific, and European cyclones (e.g., Von Ahn et al. 2005 ; Parton et al. 2010 ; Baker et al. 2013b ). Martínez
region. The term refers to Grønås's (1995) invocation of the “poisonous tail of the bent-back occlusion,” deriving from the Norwegian School's recognition of strong winds at the end of a bent-back occluded front in many cyclones that are now known as Shapiro–Keyser (1990) cyclones. Wind speed maxima resembling sting jets have been identified in other North Atlantic, North Pacific, and European cyclones (e.g., Von Ahn et al. 2005 ; Parton et al. 2010 ; Baker et al. 2013b ). Martínez
