The findings appeared in a paper authored by Courtney Schumacherand Robert Houze, atmospheric scientists at the University of Washington, Seattle, who used data from NASA's Tropical Rainfall Measuring Mission (TRMM) satellite to look at rainfall over the Pacific during the 1997-1998 El Niņo. The study was published in a recent issue of the American Meteorological Society's Journal of Climate.

El Niņo occurs when warm water shifts from the western to the eastern Pacific Ocean and trade winds that usually blow from east to west across the equator diminish. As a result, rainfall patterns around the globe change during the life of these periodic climate events, and in some areas create floods or droughts. By identifying the changes in rainfall in one area of the globe, such as the central Pacific Ocean, scientists continue to piece together the El Niņo puzzle that will help them improve rainfall forecasts around the world during the life of El Niņo.

Schumacher and Houze noticed an unusually steady rainfall over the central Pacific, much like a gray day with light rain and drizzle. That is surprising over the central Pacific, an area normally known for thunderstorms that build up during the heat of the day from rapidly rising air or convection, and then rain themselves out within an hour.

"Instead, the rainfall we saw is called 'stratiform rain,' which are weaker rains that cover larger areas," Schumacher said. It's the type of rain that makes people want to stay inside all day.

Seeing the difference between the convective and stratiform rain is very important to climatologists. Rain type matters because when water condenses and raindrops form, heat is released. That heat is a main driver in the circulation or movement of the atmosphere. "Convective rain, like from thunderstorms, releases heat lower in the atmosphere, while the steady, light, stratiform rain releases heat higher in the atmosphere," Houze said.

Heat released at different levels of the atmosphere affects the vertical and horizontal movement of air. As a result, the heat from different types of rain can alter weather patterns, such as the familiar jet stream which impacts the United States. Weather prediction models benefit from better knowledge of the changing jet stream patterns, because storms like summer thunderstorms and winter snowstorms follow the path of the jet stream.

The researchers noted that because increased stratiform rains warm the upper levels of the atmosphere, that additional heat strengthens the way air moves higher up and over a larger area than thunderstorm-generated rainfall. The larger area of air affected can impact weather patterns around the world.

Although scientists are still uncertain why such large amounts of stratiform rain happen in the middle of the Pacific, especially during El Niņo, observations from the TRMM satellite have allowed them to recognize this pattern. By identifying the type of rainfall, climatologists and meteorologists can make better rainfall forecasts in other areas of the world during the event.

"That's the beauty of NASA's TRMM satellite," said Jeff Halverson, TRMM outreach scientist from NASA's Goddard Space Flight Center, Greenbelt, Md. "TRMM can see what's happening in remote areas of the tropics that can have affects on the rest of the world."

TRMM is a joint NASA/Japanese Space Agency mission to study tropical rainfall and its implications for climate. Each day, the TRMM spacecraft observes the Earth's equatorial and tropical regions.

This research was funded by NASA's Earth Science Enterprise (ESE), the National Science Foundation and the National Oceanic and Atmospheric Administration. NASA's ESE is dedicated to understanding the Earth as an integrated system and applying Earth System Science to improve prediction of climate, weather and natural hazards using the unique vantage point of space.   For more information and images on the Internet, visit: http://www.gsfc.nasa.gov/topstory/2003/0818elNino.html

For information about TRMM on the Internet, visit: http://www.trmm.gsfc.nasa.gov

For information about AMS on the Internet, visit: http://www.ametsoc.org/AMS/