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LA NIÑA TO LAST THROUGH WINTER OF 2000
La Niña is characterized
by unusually cold sea-surface temperatures in the eastern and
central equatorial Pacific, which trigger atmospheric patterns
that influence weather around the world. For states in the Pacific
Northwest, that means wetter-than-normal conditions. Along the
southern tier, states typically experience drier, warmer conditions.
A recent weakening of the easterly trade winds in the eastern and central equatorial Pacific increased sea surface temperatures slightly, but the overall upper ocean temperature structure still indicates La Niña conditions. "In the late spring, or early summer, it's common to see some weakening in La Niña, or El Niño, but it is not an indication that the episode is going away," cautions Dr. Louis Uccellini, director of NOAA's National Centers for Environmental Prediction. Using three of its own forecast
models and the data from several others, along with information
from weather satellites and data buoys in the Pacific, NOAA scientists
have improved their understanding of oceanic and atmospheric
connections and their skills predicting the El
Niño and La Niña phenomena. NOAA accurately
forecasted months in advance the impacts of the 1997-1998 El
Niño, called the "Event of the Century," as
well as the current La Niña event. These long-range forecasts
helped communities, including farmers, city planners, emergency
and utility managers, prepare for potential, often damaging impacts.
For regular updates about La Niña on the Internet, please visit: www.cpc.ncep.noaa.gov
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