Abstract
The behavior of large-scale patterns of sea level pressure is documented using a simple composite analysis over the period 1951–85. One interpretation of the maps shows that anomalies of a given sign appear sequentially along a closed, counterclockwise trajectory that transits Asia, eastward through the tropics of the Indo-Pacific then into the eastern Pacific, and finally back to Asia via the North Pacific. A typical time scale for this process is approximately 2 yr. Unfortunately, the composites are noisy and often poorly defined, thus allowing alternate interpretations.
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CITATION STYLE
Barnett, T. P. (1988). Variations in Near-Global Sea Level Pressure: Another View. Journal of Climate, 1(2), 225–230. https://doi.org/10.1175/1520-0442(1988)001<0225:vingsl>2.0.co;2
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