Scientists from NOAA and other agencies use a variety of tools and techniques to monitor and forecast changes in the Pacific Ocean and the impact of those changes on global weather patterns. In the tropical Pacific Ocean, El Niño is detected by many methods, including satellites, moored buoys, drifting buoys, sea level analysis, and expendable buoys. Many of these ocean observing systems were part of the Tropical Ocean Global Atmosphere (TOGA) program, and are now evolving into an operational El Niño/Southern Oscillation (ENSO) observing system.
More Info![IMG]elnino.noaa.gov/images/bbox.gif[/IMG]Ka'imimoana home pageNOAA also operates a research ship, the KA'IMIMOANA, which is dedicated to servicing the Tropical Ocean Atmosphere (TAO) buoy network component of the observing system. Large computer models of the global ocean and atmosphere, such as those at the National Centers for Environmental Prediction, use data from the ENSO observing system as input to predict El Niño. Other models are used for El Niño research, such as those at NOAA's Geophysical Fluid Dynamics Laboratory, at the Center for Ocean-Land-Atmosphere Studies, and other research institutions.
Since a strong jet stream is an important ingredient for severe weather, the position of the jet stream determines the regions more likely to experience tornadoes.
More Info![IMG]elnino.noaa.gov/images/bbox.gif[/IMG]Tornado information from the National Weather Service
Contrasting El Niño and La Niña winters, the jet stream over the United States is considerably different. During El Niño the jet stream is oriented from west to east over the northern Gulf of Mexico and northern Florida. Thus this region is most susceptible to severe weather. During La Niña the jet stream extends from the central Rockies east- northeastward to the eastern Great Lakes. Thus severe weather is likely to be further north and west during La Niña than El Niño.