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Ortiz, M. J.; Ruiz De Elvira, A. (2011)
Publisher: Co-Action Publishing
Journal: Tellus A
Languages: English
Types: Article
Sea surface temperature anomalies in mid-latitude north Pacific Ocean are compared with a cyclo-stationary stochastic model in which the anomalies are forced by atmospheric “weather” disturbances. The results show that the model explains the observed two-time auto-covariances of the anomalies for almost all (98%) of the studied region.DOI: 10.1111/j.1600-0870.1985.tb00266.x
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    • Frankignoul, C. and Hasselmann, K. 1977. Stochastic climate models. Part 11. Application to sea surface temperature anomalies and thermocline variability. Tellus 29, 289-305.
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    • Frankignoul, C. & Reynolds, R. W. 1983. Testing a dynamical model for mid-latitude sea-surface temperature anomalies. J . Phys. Ocean. 13, 1131- 1145.
    • Hasselmann, K. 1976. Stochastic climate models. Part 1. Theory. Tellus 28,473-485.
    • Hasselmann, K. and Barnett. T. 1982. Techniques of linear prediction for systems with periodic statistics. J. Armos. Sci. 38. 2215-2283.
    • Lemke. P. 1977. Stochastic climate models. Part 111. Application to zonally averaged energy models. Tellus 29,385-392.
    • Lemke, P., Trinkl, E. W. and Hasselmann, K. 1980. Stochastic dynamic analysis of polar sea ice variability. J. Phys. Ocean. 10, 2 1 W 2 1 2 0 .
    • Reynolds, R. W. 1978. Sea surface temperature anomalies in the north Pacific Ocean. Tellus 30, 97-103.
    • Ruiz de Elvira. A. and Lemke, P. 1982. A Langevin equation for stochastic climate models with periodic feedback and forcing variance. Tellus 34, 3 13-320.
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