TY - JOUR
T1 - Variability of extreme precipitation in coastal river basins of the southern Mexican Pacific region
AU - Pérez-Morga, Nancy
AU - Kretzschmar, Thomas
AU - Cavazos, Tereza
AU - Smith, Stephen V.
AU - Munoz-Arriola, Francisco
N1 - Funding Information:
We are indebted to Karl-Otto Nagel who collected some of the material examined in this study. The trip of second author to Turkey was supported by the bilateral research project between University of Montenegro and University of Sinop, financed by TÜBITAK, Turkey and Ministry of Science, Montenegro.
Funding Information:
We are indebted to Karl-Otto Nagel who collected some of the material examined in this study. The trip of second author to Turkey was supported by the bilateral research project between University of Montenegro and University of Sinop, financed by TUBITAK, Turkey and Ministry of Science, Montenegro.
PY - 2013/7
Y1 - 2013/7
N2 - 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 non- tropical 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.
AB - 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 non- tropical 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.
KW - Dry years
KW - Enso
KW - Extreme rainfall events
KW - MSD
KW - PDO
KW - Tropical cyclones
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U2 - 10.1016/S0016-7169(13)71477-6
DO - 10.1016/S0016-7169(13)71477-6
M3 - Article
AN - SCOPUS:84879522814
VL - 52
SP - 277
EP - 291
JO - Geofisica International
JF - Geofisica International
SN - 0016-7169
IS - 3
ER -