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Variability of extreme precipitation in coastal river basins of the southern mexican Pacific region
Authors:Nancy Pérez-Morga  Thomas Kretzschmar  Tereza Cavazos  Stephen V Smith  Francisco Munoz-Arriola
Institution:Department of Geology, Centro de Investigación Científica y de Educación, Superior de Ensenada (CICESE), Carretera Ensenada-Tijuana Núm. 3918 Zona Playitas, Ensenada, Baja California, 22860, México.;Department of Physical Oceanography, CICESE, Ensenada, B. C., Mexico.;349 Las Flores Drive, Chula Vista, CA 91910 USA.;Department of Biological Systems Engineering., University of Nebraska-Lincoln. 246 L. W. Chase Hall., Lincoln, NE 68583-0726
Abstract:Extreme wet and dry years (± 1 standard deviation, respectively), as well as the top 95 percentile (P95) of daily precipitation events, derived from tropical cyclone (TC) and nontropical cyclone (NTC) rainfall, were analyzed in coastal river basins in Southern Oaxaca, Mexico (Río Verde, Río Tehuantepec, and the Southern Coast). The study is based on daily precipitation records from 47 quality-controlled stations for the 1961 to 1990 period and TC data for the Eastern Tropical Pacific (EPAC). The aim of this study was to evaluate extreme (dry and wet) trends in the annual contribution of daily P95 precipitation events and to determine the relationship of summer precipitation with El Niño Southern Oscillation (ENSO) and the Pacifical Decadal Oscillation (PDO). A regionalization based on a rotated principal component analysis (PCA) was used to produce four precipitation regions in the coastal river basins. A significant negative correlation (significance at the 95% level) was only found with ONI in rainfall Region 3, nearest to the Gulf of Tehuantepec. Wet years, mainly linked to TC-derived P95 precipitation events, were associated with SST anomalies (≥?0.6°C) similar to weak La Niña and Neutral cool conditions, while dry years were associated with SST positive anomalies similar to Neutral warm conditions (≤?0.5°C). The largest contribution of extreme P95 precipitation derived from TCs to the annual precipitation was observed in Region 3. A significant upward trend in the contribution of TC-derived precipitation to the annual precipitation was found only in Region 1, low Río Verde.
Keywords:eventos de lluvia extrema  MSD  años secos  ciclones tropicales  ENSO  PDO  extreme rainfall events  MSD  dry years  tropical cyclones  ENSO  PDO
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