In an earlier study of the teleconnection between streamflow and the w
arm (El Nino) phase of the El Nino/Southern Oscillation (ENSO) cycle,
we found a strong relationship evident in four regions of the United S
tates: the Gulf of Mexico, the Northeast, the North Central, and the P
acific Northwest. In this present study we have examined the same four
regions for a relationship between streamflow and the cold (La Nina)
phase of the Southern Oscillation (SO). Invariably, we found evidence
of strong and consistent streamflow responses to La Nina events within
the study regions. In each of the four regions, the strongest La Nina
signal occurred at the same time of year as had the El Nino signal in
their respective years. The sign of the seasonal streamflow anomaly a
ssociated with the La Nina events is the opposite of that associated w
ith the El Nino events. This documents the existence of the biennial t
endency related to the SO in the streamflow anomaly, which is expected
, since La Nina/El Nino are opposite phases of the ENSO cycle. Finally
, the relationships between streamflow and La Nina/El Nino were found
to be statistically significant, based on the hypergeometric distribut
ion. The results of this study demonstrate coherent, consistent, and s
ignificant midlatitude streamflow responses to the tropical SO phenome
non. This confirms the results of previous climatological studies that
have examined the extratropical teleconnections from a hydrological a
nd meteorological perspective.