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Landfalling tropical cyclones on the Pacific coast of Mexico: 1850-2010
Authors:G.B. Raga  B. Bracamontes-Ceballos  L.M. Farfán  R. Romero-Centeno
Affiliation:Centro de Ciencias de la Atmósfera, Universidad Nacional Autónoma de México, Ciudad Universitaria, 04510 México, D.F.;Facultad de Ciencias Políticas y Sociales, Universidad de Colima, Campus Norte, Km. 3.2 Carretera Colima-Guadalajara, 28010 Colima, México;Centro de Investigación Científica y de Educación Superior de Ensenada, Unidad La Paz, Miraflores 334, La Paz 23050, Baja California Sur, México;Centro de Ciencias de la Atmósfera, Universidad Nacional Autónoma de México, Ciudad Universitaria, 04510 México, D.F
Abstract:Historical documents and newspapers from Mexican Pacific states (north of 14° N) were reviewed to determine the incidence of landfalling tropical cyclones from 1850 to 1949, prior to the start of the United States National Hurricane Center database. The reviewed documents are only found in Mexican repositories at national, state and municipal level and the systematic search embarked upon in this study yielded valuable information that cannot be found elsewhere. Atime series of landfall was reconstructed back to 1850, indicating active and quiet periods. An average of 1.8 ± 1.6 landfalls per year is determined from the time series for 1850-2010. When the series is limited to 1880-2010, eliminating the first 30 years that may have some undercounting, the average increases to 2.1 ± 1.6 cases per year. Spectral and wavelet analysis of the 161 years of landfalling tropical cyclones indicates that the Pacific Decadal Oscillation (PDO) modulates the activity. The influence of El Niño/Southern Oscillation (ENSO) and the North Atlantic Oscillation (NAO) on the landfall frequency may be present throughout the reconstruction period but both oscillations have lower correlations compared to that from the PDO.
Keywords:Tropical cyclones  landfalling  Pacific coast of Mexico
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