The rush to identify El Niño, characterized by
the periodic warming of surface water temperatures off the northwestern coast of South America, as California's savior was based in part on the belief that a strong El Niño would bring as much rain as it did in the winters of 1997 - 1998 and 1982 - 1983.
El Niño is an abnormal
periodic warming of surface ocean water off the Pacific coast of South America.
Not exact matches
The climatic change at issue is known as the Atlantic Multidecadal Oscillation (AMO), a
periodic cycle
of warming and cooling
of surface temperatures in the North Atlantic.
Without the
periodic upwelling
of cold water associated with La Niña,
warm water would cover most
of the
surface of the Pacific, releasing its heat into an atmosphere already
warming because
of climate change.
For example, scientists have found that El Niño and La Niña, the
periodic warming and cooling
of surface waters in the central and eastern tropical Pacific Ocean, are correlated with a higher probability
of wet or dry conditions in different regions around the globe.
The
warm water and calm winds
of this
periodic Pacific tropical condition are «a big way to get subsurface heat back to the
surface.»
During the
warm intervals
of the middle Pliocene (3.3 to 3.0 million years ago), when there is medium confidence that global mean
surface temperatures were 2 °C to 3.5 °C
warmer than for pre-industrial climate and CO2 levels were between 250 and 450 ppm, sedimentary records suggest
periodic deglaciation
of West Antarctica and parts
of East Antarctica.