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This warm water usually dissipates to the east in non-La Niña years.
This warm water is separated from deeper, more-saline, and colder water by a shallow thermocline a layer of water between upper and lower levels that lies usually less than 100 feet (30 m) deep.
"We're expecting this warm water to peter out in the next 3 to 6 weeks," says NCEP's Anthony Barnston.
How big is this warm water in the Pacific Ocean west of Peru? "It's about 8 million square miles of overheated ocean," Patzert said.
75 percent of such systems documented between 1951 and 2000 formed near this warm water current, with two annual peaks of activity occurring during the months of May and October.
East winds moving over this warm water move warm air from over the Gulf Stream inland, helping to keep temperatures milder across the state than elsewhere across the Southeast during the winter.
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This warmer water results in melting of Antarctic ice, thereby reducing density stratification and the strength of the Antarctic Bottom Water current (AABW).
Add the warm water.
This relatively warm water species get into the Santa Barbara Basin in higher relative abundance when the California current relaxes (De Bernardi et al. 2005; De Bernardi et al. 2008; Grelaud et al. 2009b).
If you wear an Essix plastic retainer washing this with warm water may alter the shape of the tray, making it difficult or impossible to wear.
This pulls some warm water downwards, sequestering heat at greater depth.
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