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| The Effects of La Niña | |||
Changes in global atmospheric circulation patterns accompany La Niña and are responsible for weather extremes in various parts of the world that are typically opposite to those associated with El Niño. These patterns result from colder than normal ocean temperatures inhibiting the formation of rain-producing clouds over the eastern equatorial Pacific region while at the same time enhancing rainfall over the western equatorial Pacific region (Indonesia, Malaysia and northern Australia.) These patterns affect the position and intensity (weakening) of jet streams and the behavior of storms outside of the tropics in both the Northern and Southern hemispheres. The above image shows the sea surface height and temperature difference from normal during January 1999, a period of La Niña. Abnormally warm water (shown in yellow and red) expands and raises the surface of the ocean, while cool water (shown in blue) shrinks. This can be seen in the trough of cool water extending westwards from South America. (Image courtesy Greg Shirah, Scientific Visualization Studios) U.S. La Niña Impacts Global La Niña Impacts
next: NASA and NOAA Missions to Study La Niña | La Niña | ||
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