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Evan Kutta, Jason A. Hubbart, Timothy P. Eichler and Anthony R. Lupo
The El Niño-Southern Oscillation (ENSO) is a dominant source of global climate variability. The effects of this phenomenon alter the flow of heat from tropical to polar latitudes, resulting in weather and climate anomalies that are difficult to fo...
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ISMAEL PÉREZ-GARCÍA
This study explores the zonal flow in the form of Legendre polynomials. The basic flow is divided into a zonally symmetric flow and a Rossby-Haurwitz (RH) wave. Several features of this (more realistic) zonal flow make it particularly interesting, such a...
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V. MAGAÑA,T. AMBRIZZI
On the average, during boreal winter (December through February), the occurrence of El Niño/Southern Oscillation (ENSO) results in enhanced or diminished precipitation in various regions of the Americas. Anomalous convective a...
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RICHARD A. MINNICH,ERNESTO FRANCO VIZCAINO,RAYMOND J. DEZZANI
This study evaluates precipitation variability in Baja California in relation to the El Niño/Southern Oscillation (ENSO) using the Southern Oscillation Index (SOI). To evaluate precipitation climatology, data for 102 weather stations were analyzed. D...
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