A new form of El Niño has appeared on the scene. And global warming is likely to make it more common, some researchers say.
For those of us living on the US East and Gulf Coasts, the 2009 Atlantic hurricane season has been pretty quiet -- thanks in no small part to El Niño, forecasters note. (Wipe hand across forehead here.)
But over the past few years, researchers have uncovered an odd form of El Niño. Think of it as El Niño's half brother. Now, a team of atmospheric scientists from Korea, Germany, and the US suggests that this form of El Niño may become more common than the El Niños we've experienced up to now.
The likely cause of the shift? Global warming, the team says -- although other researchers caution that this half brother may be yet another form of natural variation that appears and disappears on longer time scales than El Niño does.
The team, whose results appear in the current issue of the journal Nature, posits that global warming's effect on ocean temperatures in the Pacific have changed how those temperatures shift with depth -- prompting the emergence of El Niño's half brother.
For its part, El Niño shows up as a vast pool of unusually warm ocean water that has migrated from the far western Pacific east along the equator until it bumps into South and Central America.
When such a large source of heat to the atmosphere shifts locations so dramatically, atmospheric circulation patterns shift too. So El Niño's arrival can alter seasonal rainfall, drought, and other weather patterns far from where the warm pool has docked. Indeed, a quiet North Atlantic hurricane season represents one of these "teleconnections" during an El Niño year.
El Niños crop up once every 3 to 8 years. During the "off" years, that warm pool of ocean water usually migrates back to the far western Pacific, accompanied by another set of long-range changes to atmospheric circulation patterns. This has become known as La Niña.