Ba. Malmgren et al., EL-NINO SOUTHERN OSCILLATION AND NORTH-ATLANTIC OSCILLATION CONTROL OF CLIMATE IN PUERTO-RICO, Journal of climate, 11(10), 1998, pp. 2713-2717
Many studies have shown that the El Nino-Southern Oscillation (ENSO) h
as a significant influence on climate in many parts of the globe, most
ly in the Pacific Basin. The objective of this study is to examine the
possible impact of ENSO on climatic patterns on the island of Puerto
Rico in the Caribbean. The authors find that annual mean air temperatu
res are controlled by ENSO since 1914. El Nino years are associated wi
th warm air temperatures, whereas El Viejo (La Nina) years, which are
the opposite of El Nino, are cooler. On the other hand, since 1911 flu
ctuations in annual rainfall amounts are synchronous with variations i
n the North Atlantic Oscillation (NAO) during the winter and are not c
ontrolled by ENSO. During years of a high winter NAO index, when the a
xis of moisture transport in the North Atlantic changes to a more sout
hwesterly-northeasterly orientation, annual precipitation in Puerto Ri
co is lower than average.