La Niña

Climate pattern

La Niña is a complex weather pattern resulting from variations in ocean temperatures in the Equatorial Pacific Ocean. It is one phase of the larger El Niño–Southern Oscillation (ENSO) climate pattern. La Niña is characterized by cooler than average sea surface temperatures in the central and eastern tropical Pacific Ocean.

Characteristics

La Niña events typically last between one and three years. They are associated with a number of global climatic effects, including changes in rainfall patterns, atmospheric pressure, and wind patterns. During a La Niña event, the trade winds are stronger than usual, pushing warm water towards the western Pacific and increasing the upwelling of cold water in the eastern Pacific.

Impacts

La Niña can have significant impacts on weather and climate around the world. Some of the notable effects include:

• Increased rainfall in the western Pacific, leading to flooding in countries such as Australia and Indonesia.
• Drier than normal conditions in the central and eastern Pacific, affecting regions such as the Southwestern United States and Peru.
• Enhanced hurricane activity in the Atlantic Ocean due to reduced vertical wind shear.

Monitoring and Prediction

The National Oceanic and Atmospheric Administration (NOAA) and other meteorological organizations monitor La Niña conditions using a variety of tools, including satellite observations, ocean buoys, and climate models. Predicting the onset and duration of La Niña events is crucial for preparing for their potential impacts on agriculture, water resources, and disaster management.

Related Pages

• El Niño
• Southern Oscillation
• ENSO
• Climate of the Pacific Ocean
• Weather patterns

See Also

• Climate change
• Meteorology
• Oceanography