TY - JOUR
T1 - Effects of atmospheric teleconnections on seasonal precipitation in mountainous regions of the southwestern U.S.
T2 - A case study in northern New Mexico
AU - Guan, Huade
AU - Vivoni, Enrique R.
AU - Wilson, John L.
N1 - Copyright:
Copyright 2008 Elsevier B.V., All rights reserved.
PY - 2005/12/16
Y1 - 2005/12/16
N2 - This study uses instrument records and geostatistical modeling to examine hydrologically important temporal and spatial patterns of seasonal precipitation associated with the El Niño-Southern Oscillation (ENSO) and the Pacific Decadal Oscillation (PDO) in a mountainous region of northern New Mexico. PDO is the more dominant factor, compared to ENSO, with a larger influence on winter and spring precipitation (wetter for high PDO, drier for low PDO). Extreme ENSO effects are not significant during the high PDO years, but during low PDO years El Niño strongly dampens winter and spring precipitation anomalies. Elevation modulates ENSO and PDO effects on winter anomalies, but does not seem to for other seasons. For a wetter-than-normal winter, the anomalies are larger at higher elevations, and are positive. For a drier-than-normal winter, the anomalies are larger at lower elevations, and are negative. For neutral ENSO, summer precipitation is predictable but spatially variable, indicating different local climates. High-resolution mapping brings out hydrologically important patterns of precipitation anomalies that would otherwise be blurred by spatial averaging.
AB - This study uses instrument records and geostatistical modeling to examine hydrologically important temporal and spatial patterns of seasonal precipitation associated with the El Niño-Southern Oscillation (ENSO) and the Pacific Decadal Oscillation (PDO) in a mountainous region of northern New Mexico. PDO is the more dominant factor, compared to ENSO, with a larger influence on winter and spring precipitation (wetter for high PDO, drier for low PDO). Extreme ENSO effects are not significant during the high PDO years, but during low PDO years El Niño strongly dampens winter and spring precipitation anomalies. Elevation modulates ENSO and PDO effects on winter anomalies, but does not seem to for other seasons. For a wetter-than-normal winter, the anomalies are larger at higher elevations, and are positive. For a drier-than-normal winter, the anomalies are larger at lower elevations, and are negative. For neutral ENSO, summer precipitation is predictable but spatially variable, indicating different local climates. High-resolution mapping brings out hydrologically important patterns of precipitation anomalies that would otherwise be blurred by spatial averaging.
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U2 - 10.1029/2005GL023759
DO - 10.1029/2005GL023759
M3 - Article
AN - SCOPUS:31544479045
SN - 0094-8276
VL - 32
SP - 1
EP - 4
JO - Geophysical Research Letters
JF - Geophysical Research Letters
IS - 23
M1 - L23701
ER -