What is El Niño and La Niña?
At El Niño In the generally cooler eastern Pacific Ocean along the equator, sea surface temperatures are rising by more than 3°C above the long-term average. This causes above-normal rainfall, which also reaches the west coast of South America, where it often causes catastrophic flooding. In contrast, droughts often occur in Australia, the western Pacific and India. The drop in air pressure in the eastern Pacific causes the trade winds to weaken, so that surface ocean currents and the movement of nutrient-rich water from the depths to the surface (so-called upwelling) weaken off the west coast of South America. This leads to fish kills here.
La Nina is, on the contrary, manifested by warmer sea water along the equator compared to normal by up to more than 3 °C. It causes increased precipitation in the western Pacific, and conversely drought in its central part. The increase in air pressure in the eastern Pacific causes the strengthening of the trade winds, so that the surface ocean currents and the upwelling of deep water off the western coast of South America are strengthened. The designation La Niña (little girl) arose as a contrast to the naming of the earlier known, opposite phase El Niño (little boy, baby Jesus). (CO2AI)



PARIS – After years of avoiding any explicit mention of the root cause of climate change, negotiators at the UN Climate Change Conference (COP28) in Dubai last year finally reached an agreement calling for a “transition away from fossil fuels.” But another nagging question still remains: How will this transition be financed? As Simon Stiell, the UN climate chief, recently noted, “it is clear that finance is a critical factor in the global fight against climate.” (LAURENCE TUBIANA, more at project-syndicate.org)