Scientists at NASA's Jet Propulsion Laboratory, Pasadena, Calif., studying the new data believe these abnormally warm ocean temperatures, which contrast with a cool La Nina, may be part of a larger, longer-lasting climate pattern.

The latest data, taken December 30, 1999 through January 8, 2000, show that this slower-developing condition covers most of the Pacific Ocean and has significant implications for global climate change, especially over North America, said Dr. William Patzert, an oceanographer at JPL.

"In contrast with the more spectacular but shorter duration El NiNo and La NiNa events, this multiple-year trend may be part of a decade-long pattern known as the 'Pacific decadal oscillation,'" Patzert said.

"The persistence of these abnormally high and low Pacific sea-surface patterns, along with warmer and colder than average ocean temperatures, tells us there is much more than an isolated La Ni�a occurring in the Pacific Ocean."

Satellite data from the National Oceanic and Atmospheric Administration clearly illustrate the pattern. Sea-surface temperatures, which directly affect the atmosphere on a daily basis are available and show the same warm and cool water patterns.

"These warmer and cooler than normal sea-surface temperatures influence our atmosphere every day, while sea-surface heights are a measure of how much heat is stored in the ocean below," Patzert said.

"When you put these two pieces of the climate puzzle together, they will tell us both about what is influencing today's weather and how much heat is being stored in the ocean to fuel future planetary climate events."

The Pacific decadal oscillation waxes and wanes approximately every 20 to 30 years, alternating between its present phase, with a warm horseshoe pattern of higher than normal sea-surface heights connecting the north, west and southern Pacific, in contrast to a cool wedge of lower than normal sea-surface heights in the eastern equatorial Pacific.

After that the Pacific switches to the opposite phase, showing a reversal of the warm and cool regions; the horseshoe becomes cool and the wedge warms.

The U.S.-French TOPEX/Poseidon mission is managed JPL for the NASA's Earth Science Enterprise, Washington, D.C. JPL is a division of the California Institute of Technology in Pasadena.
Source JPL

NOAA Satellite data For Sea-Surface Temperatures

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