historyPhys.org
Despite sacrificing people after catastrophic El Niño flooding, ancient societies were generally peaceful
explained
El Niño–Southern Oscillation (ENSO) is a global climate phenomenon that manifests as fluctuations in sea surface temperatures over the tropical Pacific Ocean. The warming phase of the sea surface temperature is known as "El Niño" and the cooling phase as "La Niña". It affects the climate of much of the tropics and subtropics, and has links (teleconnections) to higher-latitude regions of the world. The Southern Oscillation is the accompanying atmospheric oscillation, which is coupled with the sea temperature change. Numerous atmospheric characteristics respond to the oscillation including wind, surface air pressure and cloudiness.
The switching between El Niño, La Niña and neutral states has an irregular pattern but cycles approximately every two to seven years with varying intensity. The strength of the phenomenon tends to peak in the northern hemisphere winter, though regional impacts may peak at different times. The occurrence of ENSO is not easily predictable but it is monitored carefully by many weather organisations.
From Wikipedia: El Niño–Southern Oscillation (CC BY-SA 4.0) ↗It challenges the assumption that resource scarcity automatically leads to conflict, and it gives a useful model for how past societies responded to climate extremes.
Illustrative photo · NOAA image, Public domain, via Wikimedia Commons
