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Pacific decadal oscillation (PDO)

Posted by Administrator (admin) on 9th February, 2010
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The Pacific decadal oscillation (PDO) is a pattern of Pacific climate variability that shifts phases on at least inter-decadal time scale, usually about 20 to 30 years. The PDO is detected as warm or cool surface waters in the Pacific Ocean, north of 20° N. During a "warm", or "positive", phase, the west Pacific becomes cool and part of the eastern ocean warms; during a "cool" or "negative" phase, the opposite pattern occurs.

The Pacific (inter-)decadal oscillation was named by Steven R. Hare, who noticed it while studying salmon production patterns the results in 1997.

The mechanism by which the pattern lasts over several years has not been identified; one suggestion is that a thin layer of warm water during summer may shield deeper cold waters. A PDO signal has been reconstructed to 1661 through tree-ring chronologies in the Baja California area.[2]

The interdecadal Pacific oscillation (IPO or ID) display similar sea-surface temperature (SST) and sea-level pressure (SLP) patterns, with a cycle of 15–30 years, but affects both the north and south Pacific. In the tropical Pacific, maximum SST anomalies are found away from the equator. This is quite different from the quasi-decadal oscillation (QDO) with a period of 8-to-12 years and maximum SST anomalies straddling the equator, thus resembling the El Niño-Southern Oscillation (ENSO).

Regime shifts

Although there are several patterns of behavior, the most significant one seems to be in regime shifts between "warm" and "cool" patterns which last 5 to 20 years.

  • 1750: PDO displays an unusually strong oscillation.
  • 1905: After a strong swing, PDO changed to a "warm" phase.
  • 1946: PDO changed to a "cool" phase. [See the blue section of the graph on the right]
  • 1977: PDO changed to a "warm" phase.
  • 1998: PDO index showed several years of "cool" values, but did not remain in that pattern.
  • 2008: The early stages of a cool phase of the basin-wide Pacific Decadal Oscillation.

In all cases in the 1900s, PDO "regime shifts" were related to similar changes in the tropical ocean.

 Observed monthly values for the PDO (1900–present).
 

Reconstructed PDO (1660–1991).

Last changed: 9th February, 2010 at 17:31:31

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