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Pacific Remains Locked In Three-Year-Old Pattern: No El Nino Yet, But One Due Soon
While change may be on the way, the Pacific is still dominated by the strong, larger-than-El Nino/La Nina pattern called the Pacific Decadal Oscillation (PDO), according to the latest data from the U.S.-French TOPEX/Poseidon satellite mission, managed by NASA's Jet Propulsion Laboratory, Pasadena, Calif. The PDO is a long-term ocean temperature fluctuation of the Pacific Ocean that waxes and wanes approximately every 10 to 20 years. "This continuing PDO pattern of the past three years signals more of the unusually dry conditions that have afflicted the North American west coast," said JPL oceanographer Dr. William Patzert. The new satellite image shows a pulse of warm water traveling toward South America, a reminder that another El Nino is due in the next year or so. El Ninos generally return every two to seven years; the last one occurred in 1997. This equatorial, eastward-traveling Kelvin wave (a bulge of warm water) is headed toward South America at about 140 degrees West longitude. In late July, when this wave arrives at the west coast of South America, there should be a modest warming of the eastern Pacific. Kelvin waves, often seen before an El Nino develops, are triggered by westerly wind bursts (i.e., winds blowing in the opposite direction from the normal easterly trade winds) in the western Pacific. Also, the strength of El Nino's next appearance could depend on how much the PDO dominates ocean circulation and temperature patterns over the next few years. The data were taken during a 10-day collection cycle ending June 11, 2001. They show that the near-equatorial ocean has slowly warmed in the past year and sea levels and sea- surface temperatures are near normal. Above-normal sea- surface heights and warmer ocean temperatures (indicated by the red and white areas) still blanket the far-western tropical Pacific and much of the north and south mid- Pacific. Red areas are about 10 centimeters (4 inches) above normal; white areas show the sea-surface height is between 14 and 32 centimeters (6 to 13 inches) above normal. In the Western Pacific, the build-up of heat, first noted by TOPEX/Poseidon oceanographers more than two years ago, has outlasted the La Nina of the past few years. This warmth contrasts with the Bering Sea, Gulf of Alaska and U.S. West Coast where lower-than-normal sea surface levels and cool ocean temperatures continue (indicated by blue areas). The blue areas are between 5 and 13 centimeters (2 and 5 inches) below normal, whereas the purple areas range from 14 to18 centimeters (6 to 7 inches) below normal. For now, these latest TOPEX/Poseidon data show that the entire Pacific basin continues to be dominated by the strong and stable PDO's characteristic warm horseshoe and cool wedge pattern. Most recent National Oceanic and Atmospheric Administration (NOAA) sea-surface temperature data also clearly illustrate the persistence of this basin-wide pattern as shown here. "Given the three-year persistence of the PDO pattern, there will be a tendency to produce impacts similar to the past two summers with continuing drought and heat in the West," said Patzert. "In some parts of the West, this long- lasting drought has created considerable pain. In the Pacific Northwest, water supplies are dangerously low and temperatures should be up, which will exacerbate the energy crisis and, like the summer of 2000, we are set up for a very busy summer and fall fire season," said Patzert. "Warm oceanic patterns in the North Pacific and tropical Atlantic suggest a more-active-than-normal hurricane season for the U.S. East and Gulf Coasts. The only good news in this is that the Gulf Coast and Florida could sure use the rainfall, but the danger is that it could come as the recent costly and painful deluge of tropical storm Allison," said Patzert. Related Links TOPEX/Poseidon SpaceWar Search SpaceWar Subscribe To SpaceWar Express 
Finding El Nino's Trigger Event
Washington - Feb. 5, 2001Just as a spark can grow into a fire, so small departures of winds from the normal seasonal cycle in the far western equatorial Pacific can trigger a full-blown El Nino. Writing in the February 15 issue of the journal Geophysical Research Letters, Prof. Allan J. Clarke and Research Associate Stephen Van Gorder of Florida State University describe the model they have developed to predict El Nino using this trigger.
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