skip to main content
OSTI.GOV title logo U.S. Department of Energy
Office of Scientific and Technical Information

Title: Prediction of tropical Atlantic sea surface temperatures using linear inverse modeling

Journal Article · · Journal of Climate
;  [1]
  1. Univ. of Colorado, Boulder, CO (United States)

The predictability of tropical Atlantic sea surface temperature on seasonal to interannual timescales by linear inverse modeling is quantified. The authors find that predictability of Caribbean Sea and north tropical Atlantic sea surface temperature anomalies (SSTAs) is enhanced when one uses global tropical SSTAs as predictors compared with using only tropical Atlantic predictors. This predictability advantage does not carry over into the equatorial and south tropical Atlantic; indeed, persistence is a competitive predictor in those regions. To help resolve the issue of whether or not the dipole structure found by applying empirical orthogonal function analysis to tropical Atlantic SSTs is an artifact of the technique or a physically real structure, the authors combine empirically derived normal modes and their adjoints to form influence functions, maps highlighting the geographical areas to which the north tropical Atlantic and the south tropical Atlantic SSTs are most sensitive at specified lead times. When the analysis is confined to the Atlantic basin, the 6-month influence functions in the north and south tropical Atlantic tend to be of the opposite sign and evolve into clear dipoles within 6 months. When the analysis is performed on global tropical SSTs, the 6-month influence functions are connected to the El Nino phenomenon in the Pacific, with the strongest signal in the north tropical Atlantic. That is, while the south tropical Atlantic region is weakly sensitive to the optimal initial structure for growth of El Nino, SST anomaly in the Nino 3 region is a strong 6-month predictor of SST anomaly in the north tropical Atlantic. The results suggest that the tropical Atlantic dipole is a real phenomenon rather than an artifact of EOF analysis but that the influence of the Indo-Pacific often disrupts the northern branch so that the dipole does not dominate tropical Atlantic dynamics on seasonal timescales. 38 refs., 12 figs., 1 tab.

OSTI ID:
621419
Journal Information:
Journal of Climate, Vol. 11, Issue 3; Other Information: PBD: Mar 1998
Country of Publication:
United States
Language:
English

Similar Records

Extreme Rainfall Variability in Australia: Patterns, Drivers, and Predictability*
Journal Article · Tue Jul 29 00:00:00 EDT 2014 · Journal of Climate · OSTI ID:621419

Analysis of the 1877-78 ENSO episode and comparison with 1982-83
Journal Article · Sun Jun 01 00:00:00 EDT 1986 · Mon. Weather Rev.; (United States) · OSTI ID:621419

The global climate for March-May 1993: Mature ENSO conditions persist and a blizzard blankets the eastern United States
Journal Article · Tue Nov 01 00:00:00 EST 1994 · Journal of Climate · OSTI ID:621419