answersLogoWhite

0

The El Niño-Southern Oscillation (ENSO) is a naturally occurring phenomenon that involves fluctuating ocean temperatures in the equatorial Pacific. The warmer waters essentially slosh, or oscillate, back and forth across the Pacific, much like water in a bath tub.

User Avatar

Wiki User

9y ago

What else can I help you with?

Continue Learning about Earth Science

What does ENSO mean?

ENSO stands for El Niño-Southern Oscillation, a climate phenomenon characterized by the periodic warming (El Niño) and cooling (La Niña) of sea surface temperatures in the central and eastern tropical Pacific Ocean. ENSO can have significant impacts on weather patterns worldwide, influencing things like rainfall, temperature, and storm activity.


What does ENSO stand for?

ENSO stands for El Niño Southern Oscillation. It is a climate pattern that occurs in the tropical Pacific Ocean, characterized by the warming (El Niño) and cooling (La Niña) of sea surface temperatures, which can have significant impacts on weather patterns around the world.


What is an occasional climate event that occurs every 3-8 years?

An example of an occasional climate event that occurs every 3-8 years is the El Niño Southern Oscillation (ENSO). It is a climate pattern that involves the periodic warming of sea surface temperatures in the central and eastern tropical Pacific Ocean, leading to significant impacts on weather patterns worldwide.


Why a phenomenan similar to El Niño?

A phenomenon similar to El Niño is known as La Niña, which is characterized by cooler than normal sea surface temperatures in the central and eastern tropical Pacific Ocean. La Niña typically brings opposite impacts compared to El Niño, such as increased rainfall in the western Pacific and drier conditions in the eastern Pacific. Both El Niño and La Niña are part of the El Niño-Southern Oscillation (ENSO) climate pattern.


What is the Madden Julian oscillation?

The MJO is a coupling between atmospheric circulation and deep tropical convection which tends to have a period of variability of 1-3 months. It is characterized by tropical convection propogating eastward, starting in the Indian Ocean and moving through the Pacific Ocean. It is linked to other modes of low frequency variability such as ENSO, but is not necessarily causal. Its impacts include primarily rainfall anomalies in parts of the Eastern tropics, and more subtle effects on moisture and energy getting into the mid- and high latitudes. It is displayed using a Hovmöller diagram.