The Pacific Decadal Oscillation (PDO) is often described as a long-lived El Niño-like pattern of Pacific climate variability (Zhang et al. 1997). As seen with the better-known El Niño/Southern Oscillation (ENSO), extremes in the PDO pattern are marked by widespread variations in the Pacific Basin and the North American climate.

Pacific Decadal Oscillation (PDO) Describes SST variability in the north Pacific Ocean. Correlation of the PDO from NOAA/PSL with the NOAA ERSST V5 SST for January

2022年9月9日 · The Pacific Decadal Oscillation (PDO) is defined by the leading pattern (EOF) of sea surface temperature (SST) anomalies in the North Pacific basin (typically, polewards of 20°N). The SST anomalies are obtained by removing both the climatological annual cycle and the global-mean SST anomaly from the data at each gridpoint.

Two main characteristics distinguish PDO from El Niño/Southern Oscillation (ENSO): first, 20th century PDO "events" persisted for 20-to-30 years, while typical ENSO events persisted for 6 to 18 months; second, the climatic fingerprints of the PDO are most visible in the North Pacific/North American sector, while secondary signatures exist in ...

1948 2022 1948 -0.11 -0.74 -0.03 -1.33 -0.23 0.08 -0.92 -1.56 -1.74 -1.32 -0.89 -1.70 1949 -2.01 -3.60 -1.00 -0.53 -1.07 -0.70 -0.56 -1.30 -0.93 -1.41 -0.83 -0.80 1950 -2.13 -2.91 -1.13 -1.20 -2.23 -1.77 -2.93 -0.70 -2.14 -1.36 -2.46 -0.76 1951 -1.54 -1.06 -1.90 -0.36 -0.25 -1.09 0.70 -1.37 -0.08 -0.32 -0.28 -1.68 1952 -2.01 -0.46 -0.63 -1.05 ...

The Pacific Decadal Oscillation (PDO) is a long-term ocean fluctuation of the Pacific Ocean. The PDO waxes and wanes approximately every 20 to 30 years. From ocean surface topography data, together with other ocean and atmospheric data, scientists can determine whether we are in a ‘cool’ phase or a ‘warm’ phase.

PDO INDEX If the columns of the table appear without formatting on your browser, use http://research.jisao.washington.edu/pdo/PDO.latest.txt Updated standardized values for the PDO index, derived as the leading PC of monthly SST anomalies in the …

The PDO is a long-term (10-20 year) oscillation of the Pacific Ocean in response to the changes in the atmosphere. During a warm (positive) phase, the response of the ocean to low atmospheric pressure over the Aleutian Islands causes ocean currents to bring warm waters in the Eastern Pacific Ocean and along the coast of North America and cool ...

The Pacific Decadal Oscillation (PDO) is an SST anomaly pattern of Pacific climate variability that shifts phases on an inter-decadal time scale usually covering more than 10 years. The PDO index is defined as the projections of monthly mean SST anomalies onto their first EOF vectors in the North Pacific (north of 20ºN).

The Pacific Decadal Oscillation (PDO) is often described as a long-lived El Niño-like pattern of Pacific climate variability (Zhang et al. 1997). As seen with the better-known El Niño/Southern Oscillation (ENSO), extremes in the PDO pattern are marked by widespread variations in the Pacific Basin and the North American climate.