el nino southern oscillation Sentence Examples
- El Niño Southern Oscillation (ENSO) is a climate phenomenon that occurs in the Pacific Ocean.
- It causes large-scale changes in temperature and precipitation patterns around the world.
- El Niño is the warm phase of ENSO, characterized by unusually high sea surface temperatures in the central and eastern Pacific.
- La Niña is the cool phase of ENSO, characterized by unusually low sea surface temperatures in the central and eastern Pacific.
- The El Niño phase is typically associated with wetter conditions in the Americas, Australia, and Southeast Asia.
- The La Niña phase is typically associated with drier conditions in the Americas, Australia, and Southeast Asia.
- ENSO can also have impacts on the global economy, with severe events leading to flooding, droughts, and other natural disasters.
- Scientists are working to better understand ENSO and its impacts in order to improve forecasting and preparedness.
- Climate change is expected to lead to more frequent and intense El Niño and La Niña events.
- The impacts of ENSO are a reminder of the interconnectedness of the Earth's climate system.
el nino southern oscillation Meaning
el nino southern oscillation (n)
a more intense El Nino that occurs every few years when the welling up of cold nutrient-rich water does not occur; kills plankton and fish and affects weather patterns
Synonyms & Antonyms of el nino southern oscillation
No Synonyms and anytonyms found
FAQs About the word el nino southern oscillation
a more intense El Nino that occurs every few years when the welling up of cold nutrient-rich water does not occur; kills plankton and fish and affects weather p
No synonyms found.
No antonyms found.
El Niño Southern Oscillation (ENSO) is a climate phenomenon that occurs in the Pacific Ocean.
It causes large-scale changes in temperature and precipitation patterns around the world.
El Niño is the warm phase of ENSO, characterized by unusually high sea surface temperatures in the central and eastern Pacific.
La Niña is the cool phase of ENSO, characterized by unusually low sea surface temperatures in the central and eastern Pacific.
