On April 4, the President of Zimbabwe, Emmerson Mnangagwa, declared a "State of Drought Disaster" due to the "severe food situation caused by the El Nino effect."
Zambia and Malawi had already declared a disaster as El Nino-driven drought continued to devastate crops across southern Africa.
This El Nino cycle, which scientists say began around June and peaked in December before starting to wane, is also behind extreme heat and drought in Southeast Asia — including in the Philippines, where schools have been forced to shut because of record temperatures.
Its "little girl" sister, La Nina, creates weather patterns that, although variable, tend to be wetter and lead to intense storms and hurricanes.
Zimbabwe declares drought-induced state of disaster
How El Nino causes weather extremes
The El Nino weather phase is part of the so-called El Nino-Southern Oscillation (ENSO), a climate pattern triggered in the Pacific Ocean.
El Nino commonly occurs every two to seven years when regular trade winds moving east-west across the Pacific weaken and sometimes even reverse.
These winds usually blow across the equator and take warm water from South America toward Southeast Asia and Australia.
But, when the winds start to calm, the warmer water remains in South America and fails to travel west. As the warmth suppresses the usual upwelling of cold water in the eastern Pacific, extra heat in the atmosphere typically supercharges regional rainfall and causes flooding in northern South American countries such as Bolivia.
Meanwhile, the absence of warm water in the western Pacific can result in drought and extreme temperatures.
Though predictions of a nightmare fire season in Australia in the summer of 2023-24 at the peak of the El Nino cycle did not come to pass, August through October were still the driest months in 120 years.
El Niño-induced drought hits Southern Africa's agricultural sector
El Nino's disruption of ocean heat can alter the path of jet streams — strong winds far above the ground — that travel the planet, guiding rains. This causes broad climate disruption, including the stalling of the monsoon in Indonesia and India, but also the reduction of hurricane activity in the Atlantic.
Furthermore, El Nino was partly to blame for heavy rains and flooding in East Africa in late 2023. By late last year, floods had killed 120 people and displaced 700,000 residents in Kenya.
Though researchers have found that the direct impact of El Nino on rainfall in eastern African is relatively modest, they say it can kick-start a positive Indian Ocean Dipole, another climate pattern that is bringing extreme flooding to the region.
La Nina fuels storms and hurricanes
La Nina, another key phase in the ENSO, has the opposite impact from El Nino as predominant east-west winds become stronger than usual.
An increase of warmer water in the west brings increased rainfall to Australia and Southeast Asia.
La Nina phases can spark drought and wildfires in eastern Pacific regions from southwestern United States and Mexico through to South America. However, regional variability means that northeast US states and Canada tendi to be wetter and colder during La Nina winters.
La Nina also typically enhances hurricane activity in the Atlantic Basin, a phenomenon that is being exacerbated by record warm ocean surface temperatures in the Atlantic.
Impacts are hard to predict
Though La Nina and El Nino are natural patterns, their relative impacts can vary depending on their timing, duration and complex climate influences that include human-induced global heating.
There is some evidence that climate change has made ENSO events more frequent and intense.
Scientists say El Nino and La Nina cycles are likely to hit harder as the planet heats up. Hotter air holds more water and causes more extreme rainfall.
Researchers add that achieving net-zero greenhouse gas emissions through the phasing out of fossil fuels has the potential to limit both global heating and ENSO impacts.
