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NOAA climate scientists expect El Niño conditions to strengthen during the winter of 2009-2010 and continue into the spring of 2010. El Niño By Diana Hayden and Jon Mittelstadt is a phenomenon in the equatorial Pacific Ocean characterized by a positive sea surface temperature departure from normal averaged over three months.
10 Αυγ 2011 · The latest El Niño event in 2009–2010, which is classified as warm pool El Niño, holds a unique ground in that it marks the strongest warming signal in the central Pacific but rapidly decays to str...
17 Αυγ 2011 · Highlights. In 2010, the El Niño-Southern Oscillation ("ENSO," for short) climate pattern swung first through its warm phase and then its cool phase, with significant influences on seasonal climate around the globe.
A moderate El Niño event developed in the fall of 2009 and persisted through the winter. The sea surface temperature anomalies from 2000 through 2010 in the Niño 3.4 region of the tropical Pacific Ocean (Figure 1) indicate that this event was of similar strength to the 2002-2003 El Niño.
1 Αυγ 2011 · The latest El Niño event in 2009-2010, which is classified as warm pool El Niño, holds a unique ground in that it marks the strongest warming signal in the central Pacific but rapidly decays to...
4 Ιουν 2011 · During the winter of 2009–2010, the El Niño Modoki type warming in the central Pacific, prominently affected the climate of the Northern Hemisphere. Most of those resulted regional anomalies appear similar to what was observed in previous Modoki years (Ashok et al. 2007, Weng et al. 2009).
El Niño is a phenomenon that occurs when unusually warm ocean water piles up along the equatorial west coast of South America. When this phenomenon develops, it affects weather patterns around the globe, including the winter weather along the west coast of North America.
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