Northern hemisphere tropical cyclones during the quasi-El Niño of late 2014

• Main Authors: Sobel, Adam H., Camargo, Suzana J., Barnston, Anthony G., Tippett, Michael K.
• Format: Text
• Language: unknown
• Published: Columbia University 2016
• Subjects: Climatology; Cyclones; Southern oscillation; Pacific; North Atlantic
• Online Access: https://dx.doi.org/10.7916/d8-9vmt-6129; https://academiccommons.columbia.edu/doi/10.7916/d8-9vmt-6129

During the second half of 2014, the tropical Pacific was in a state marginally consistent with El Niño. While oceanic indicators were indicative of a weak El Niño event, a number of atmospheric indicators were not, and a number of forecast centers did not declare an El Niño. Nonetheless, the most active tropical cyclone basins of the northern hemisphere—those of the North Atlantic and Pacific—showed tropical cyclone statistics that in some respects were consistent with El Niño. In particular, the numbers of relatively intense storms in the four basins considered—major hurricanes in the Eastern North Pacific and North Atlantic, super typhoons in the Western North Pacific, and hurricanes in the Central North Pacific—formed a pattern strongly consistent with El Niño.