4  PDO (Pacific Decadal Oscillation)

Description The CCLME is driven by atmosphere–ocean energy exchange that occurs on many temporal and spatial scales. The Pacific Decadal Oscillation (PDO, Mantua et al. (1997)) describes North Pacific sea surface temperature (SST) anomalies that may persist for many years. Positive PDOs are associated with warmer SST and lower productivity in the CCE, while negative PDOs indicate cooler SST and are associated with higher productivity.

Pacific Decadal Oscillation Index

Indicator Download

ERDDAP™ link:

https://oceanview.pfeg.noaa.gov/erddap/tabledap/cciea_OC_PDO.html

References

Huang, Boyin, Peter W. Thorne, Viva F. Banzon, Tim Boyer, Gennady Chepurin, Jay H. Lawrimore, Matthew J. Menne, Thomas M. Smith, Russell S. Vose, and Huai-Min Zhang. 2017. “Extended Reconstructed Sea Surface Temperature, Version 5 (ERSSTv5): Upgrades, Validations, and Intercomparisons.” Journal of Climate 30 (20): 8179–8205. https://doi.org/10.1175/JCLI-D-16-0836.1.
Mantua, Nathan J., Steven R. Hare, Yuan Zhang, John M. Wallace, and Robert C. Francis. 1997. “A Pacific Interdecadal Climate Oscillation with Impacts on Salmon Production.” Bulletin of the American Meteorological Society 78 (6): 1069–79. https://doi.org/10.1175/1520-0477(1997)078<1069:apicow>2.0.co;2.
Smith, Thomas M., Richard W. Reynolds, Thomas C. Peterson, and Jay Lawrimore. 2008. “Improvements to NOAA’s Historical Merged Land-Ocean Surface Temperature Analysis (1880-2006).” Journal of Climate 21 (10): 2283–96. https://doi.org/10.1175/2007JCLI2100.1.
Wen, C, A Kumar, and Y Xue. 2014. “Factors Contributing to Uncertainty in Pacific Decadal Oscillation Index.” Geophys. Res. Lett. 41: 7980–86. https://doi.org/10.1002/2014GL061992.