Por |
Montecinos, A; Kurgansky, M; Muñoz, C; Takahashi, Ken
(Instituto Geofísico del Perú, 2011-01-15)
"The first principal component (PC1) of seasonal rainfall anomalies in central Chile during winter (June–August) is used to analyze the circulation anomalies related
to wet and dry conditions, when near-normal or neutral SST anomalies are observed in the equatorial Pacific, i.e., during non-ENSO ...