phenomenon

Niño 1+2

The coastal patch off Peru and Ecuador (0 to 10°S, 90 to 80°W). The easternmost of the four.
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Description

The Niño 1 and 2 region is a small coastal area off the shores of Peru and Ecuador, bounded by 0° to 10°S latitude and 90°W to 80°W longitude. It is the easternmost of the four Niño index regions, hugging the South American continent where the cold Humboldt Current normally brings nutrient-rich waters to the surface. This patch is the first place where the early signs of an El Niño often appear, as warm water pools along the coast and disrupts the usual upwelling.

History

This index was among the earliest used by Peruvian fishermen and scientists in the 20th century to describe the annual warm current they called 'El Niño' (the Christ Child), as it often appeared around Christmas.

How it works

The region's temperature is measured from coastal stations and satellite observations. During El Niño, the trade winds weaken, allowing warm western Pacific water to slosh eastward and pile up here, raising sea-surface temperatures by several degrees. Because the area is small and shallow, it responds quickly to changes in wind and ocean currents, making it a sensitive early-warning zone for the onset of a broader El Niño event.

In practice

It is used to monitor coastal impacts such as marine ecosystem disruption, fish migration, and heavy rainfall that can trigger flooding and landslides in Peru and Ecuador.

Fun fact

The region's warm anomalies can be so strong that they cause massive die-offs of anchovies and guano birds, collapsing the local fishing industry within weeks.

Concept graph →

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