Pacific decadal oscillation: Tropical Pacific forcing versus internal variability

TitlePacific decadal oscillation: Tropical Pacific forcing versus internal variability
Publication TypeJournal Article
Year of Publication2018
AuthorsZhang Y., Xie SP, Kosaka Y, Yang J.C
JournalJournal of Climate
Volume31
Pagination8265-8279
Date Published2018/10
Type of ArticleArticle
ISBN Number0894-8755
Accession NumberWOS:000443673000006
KeywordsClimate variability; enso; geopotential height; global-warming hiatus; hemisphere circulation; Meteorology & Atmospheric Sciences; north pacific; Pacific decadal oscillation; part i; sea-surface temperature; southern-oscillation; teleconnections
Abstract

The Pacific decadal oscillation (PDO) is the leading mode of sea surface temperature (SST) variability over the North Pacific (north of 20 degrees N). Its South Pacific counterpart (south of 20 degrees S) is the South Pacific decadal oscillation (SPDO). The effects of tropical eastern Pacific (TEP) SST forcing and internal atmospheric variability are investigated for both the PDO and SPDO using a 10-member ensemble tropical Pacific pacemaker experiment. Each member is forced by the historical radiative forcing and observed SST anomalies in the TEP region. Outside the TEP region, the ocean and atmosphere are fully coupled and freely evolve. The TEP-forced PDO (54% variance) and SPDO (46% variance) are correlated in time and exhibit a symmetric structure about the equator, driven by the Pacific-North American (PNA) and Pacific-South American teleconnections, respectively. The internal PDO resembles the TEP-forced component but is related to internal Aleutian low (AL) variability associated with the Northern Hemisphere annular mode and PNA pattern. The internal variability is locally enhanced by barotropic energy conversion in the westerly jet exit region around the Aleutians. By contrast, barotropic energy conversion is weak associated with the internal SPDO, resulting in weak geographical preference of sea level pressure variability. Therefore, the internal SPDO differs from the TEP-forced component, featuring SST anomalies along similar to 60 degrees S in association with the Southern Hemisphere annular mode. The limitations on isolating the internal component from observations are discussed. Specifically, internal PDO variability appears to contribute significantly to the North Pacific regime shift in the 1940s.

DOI10.1175/jcli-d-18-0164.1
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