decadal climate variation
Quick Summary
Decadal climate variation refers to climate shifts that occur over periods of ten years or more, characterized by multiyear clusters of wet, dry, cool, or warm conditions. These variations can significantly impact human activities and well-being, as seen in historical examples of droughts affecting civilizations.1
The causes of decadal climate variation are complex and are thought to arise from interactions between the ocean and atmosphere. Phenomena like the Pacific Decadal Oscillation (PDO) and the Atlantic Multidecadal Oscillation (AMO) are examples of such ocean-atmosphere interactions that influence precipitation patterns over large regions. While interannual variations, such as El Niño-Southern Oscillation (ENSO), are more frequent, decadal variations represent longer-term shifts in climate patterns. Understanding these decadal changes is a key area of study for climatologists.12
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