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- 2de06b90-4abe-4c71-a537-978679bf8aea type Model @default.
- 2de06b90-4abe-4c71-a537-978679bf8aea type Science_Keyword @default.
- 2de06b90-4abe-4c71-a537-978679bf8aea broader 1eb0ea0a-312c-4d74-8d42-6f1ad758f999 @default.
- 2de06b90-4abe-4c71-a537-978679bf8aea broader 23703b6b-ee15-4512-b5b2-f441547e2edf @default.
- 2de06b90-4abe-4c71-a537-978679bf8aea broader 5273c8c2-d30b-4666-b2d5-0388ce2741d0 @default.
- 2de06b90-4abe-4c71-a537-978679bf8aea broader b887d3e5-4280-43d2-a34e-0f63ac086b6a @default.
- 2de06b90-4abe-4c71-a537-978679bf8aea broader e9f67a66-e9fc-435c-b720-ae32a2c3d8f5 @default.
- 2de06b90-4abe-4c71-a537-978679bf8aea definition "Fisheries scientist Steven Hare coined the term Pacific DecadalOscillation PDO in 1996 while researching connections betweenAlaska salmon production cycles and Pacific climate PDO has sincebeen described as a longlived El Ninolike pattern of Pacificclimate variability because the two climate oscillations have similarspatial climate fingerprints but very different temporal behaviorTwo main characteristics distinguish PDO from El Nino SouthernOscillation ENSO first 20th century PDO events persisted for20to30 years while typical ENSO events persisted for 6 to 18months second the climatic fingerprints of the PDO are most visiblein the North PacificNorth American sector while secondary signaturesexist in the tropics the opposite is true for ENSOSeveral independent studies find evidence for just two full PDO cyclesin the past century cool PDO regimes prevailed from 18901924 andagain from 19471976 whilewarm PDO regimes dominated from 19251946and from 1977 through at least the mid1990s Shoshiro Minobe hasshown that 20th century PDO fluctuations were most energetic in twogeneral periodicities one from 15to25 years and the other from50to70 years" @default.
- 2de06b90-4abe-4c71-a537-978679bf8aea prefLabel "PACIFIC_DECADAL_OSCILLATION" @default.