Article Type:
Research Article

Investigation of a Large-Scale Mode of Ocean–Atmosphere Variability and Its Relation to Tropical Pacific Sea Surface Temperature Anomalies

Bruce T. Anderson Department of Geography, Boston University, Boston, Massachusetts

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Print Publication:
15 Oct 2004
DOI:
https://doi.org/10.1175/1520-0442(2004)017<4089:IOALMO>2.0.CO;2
Page(s):
4089–4098
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Abstract

By examining the linearly coupled atmospheric and oceanic signals related to interannual variability in sea surface temperatures and upper-air wind fields, a hemispheric-scale ocean–atmosphere teleconnection mode is isolated that is significantly correlated with equatorial Pacific SSTs 12 months later. The interannual component of this teleconnection mode is related to a basin-scale dipole in the upper-air wind fields stretching across the extratropical Pacific, with additional anomalies extending from the eastern tropical Pacific over North America and into the Atlantic basin. In addition, it is related to variability in the SST field with warm anomalies found over the tropical/subtropical western Pacific as well as the equatorial eastern Pacific; also, there are related cold anomalies over the extratropical central North Pacific that extend down into the central subtropical/tropical Pacific. Diagnostic studies investigating the ocean–atmosphere structure for this mode of variability indicate that the large-scale variations in the upper-air circulation patterns are associated with anomalous equatorward propagation of transient and stationary wave activity over the North Pacific. In addition, they are characterized by vertical circulation patterns over both the subtropical and extratropical Pacific, which are collocated with variations in surface pressure and wind stress fields over the central subtropical and tropical North Pacific. Previous research has shown that modifications of these two fields are significantly related to the evolution of equatorial Pacific SSTs and may provide the dynamic mechanism whereby the ocean–atmosphere teleconnection mode described here influences the development of the ENSO system. This influence appears to be related to a modification of the basin-scale heat content over the central and eastern tropical Pacific; however, significant discussion is provided concerning alternative hypotheses.

Corresponding author address: Bruce T. Anderson, Department of Geography, Boston University, 675 Commonwealth Ave., Boston, MA 02215-1401. Email: brucea@bu.edu

Abstract

By examining the linearly coupled atmospheric and oceanic signals related to interannual variability in sea surface temperatures and upper-air wind fields, a hemispheric-scale ocean–atmosphere teleconnection mode is isolated that is significantly correlated with equatorial Pacific SSTs 12 months later. The interannual component of this teleconnection mode is related to a basin-scale dipole in the upper-air wind fields stretching across the extratropical Pacific, with additional anomalies extending from the eastern tropical Pacific over North America and into the Atlantic basin. In addition, it is related to variability in the SST field with warm anomalies found over the tropical/subtropical western Pacific as well as the equatorial eastern Pacific; also, there are related cold anomalies over the extratropical central North Pacific that extend down into the central subtropical/tropical Pacific. Diagnostic studies investigating the ocean–atmosphere structure for this mode of variability indicate that the large-scale variations in the upper-air circulation patterns are associated with anomalous equatorward propagation of transient and stationary wave activity over the North Pacific. In addition, they are characterized by vertical circulation patterns over both the subtropical and extratropical Pacific, which are collocated with variations in surface pressure and wind stress fields over the central subtropical and tropical North Pacific. Previous research has shown that modifications of these two fields are significantly related to the evolution of equatorial Pacific SSTs and may provide the dynamic mechanism whereby the ocean–atmosphere teleconnection mode described here influences the development of the ENSO system. This influence appears to be related to a modification of the basin-scale heat content over the central and eastern tropical Pacific; however, significant discussion is provided concerning alternative hypotheses.

Corresponding author address: Bruce T. Anderson, Department of Geography, Boston University, 675 Commonwealth Ave., Boston, MA 02215-1401. Email: brucea@bu.edu

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