El Niño has a little brother, Atlantic Niño, who lives just across the South American continent, in the equatorial Atlantic Ocean.
Like El Niño, Atlantic Niño is characterized by warmer-than-average sea surface temperatures in the eastern equatorial basin, and weaker-than-average
trade winds, throughout the east-central equatorial Atlantic.
Atlantic Niño, in contrast to El Niño, tends to peak in summer when ENSO is usually inactive, is usually shorter in duration, is overall much weaker than ENSO, and has more modest and local climate impacts.
For example, Atlantic Niño often disrupts the West African summer monsoon, leading to reduced rainfall in the Sahel region, and is linked to increased frequency of flooding in northeastern
South America and the West African sub-Sahel countries bordering the Gulf of Guinea.
The atmosphere-ocean feedback responsible for the onset of Atlantic Niño is believed to be similar to that of El Niño, a process known as Bjerknes feedback (BF). Recent studies have shown a weakening of the Atlantic Niño variability in the past decades. The changes in eastern equatorial Atlantic SST variability have been attributed to the combined effect of a weakening of the Bjerknes feedback, and increased latent heat flux damping, and to a basin-wide warming, related to climate change.
The Atlantic Niño is just one
member of a big extended
family that covers much of the tropical and subtropical oceans.
Just like El Niño, Atlantic Niño has a sister, Atlantic Niña, that brings cooler-than-average equatorial Atlantic conditions and the opposite climate impacts as her brother. There are many other siblings , cousins, and distant relatives spanning the Pacific, Atlantic, and Indian Oceans, who share a feature in common: ocean surface temperature anomalies, along eastern boundaries, linked to changes in the upwelling of cooler
water from below.
The underlying Bjerknes feedback mechanism consists of three components:
a) a weakening of the equatorial trades (westerly
wind anomalies) in the western basin deepens the thermocline in the east;
b) the deepened thermocline reduces upwelling efficiency and warms sea-surface temperature (SST) in the east;
c) warm SSTs further weaken the equatorial trades. Various studies have suggested that a similar feedback mechanism operates in the equatorial Atlantic.
The latent heat flux (Fl) is the exchange of energy between the sea surface and the atmosphere, that occurs when
water is evaporated from, or condenses onto, the sea surface.
There are four more relatives in the
Atlantic Ocean, Benguela Niño/Niña along the coast of Angola and Namibia, and Dakar Niño/Niña along the
east coast of West
Africa.
There are four more in the Pacific,
California Niño/Niña and
Chile Niño/Niña along the
California and Chilean coasts, respectively.
In the
Indian Ocean, only two have been found so far, Ningaloo Niño/Niña off the
west coast of
Australia.