Titlebook: Decadal Climate Variability; Dynamics and Predict David L. T. Anderson,Jürgen Willebrand Conference proceedings 1996 Springer-Verlag Berlin

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Mechanisms for Decadal-to-Centennial Climate Variability,f this type, so it is hoped that these lectures will serve as a guide to the ideas and literature of a field that is rapidly catching on as the realization takes hold that natural variability of the climate is omnipresent and important, and may be predictable.

FLIRT

Long-Term Coordinated Changes in the Convective Activity of the North Atlantic,g Lazier,1980 et seq.), and at the PANULIRUS / Hydrostation “S” site in the Northern Sargasso off Bermuda (eg Jenkins, 1982, Talley and Raymer, 1982). This paper reviews the recent history of these changes showing that the major convective centres of the Greenland- and Labrador Seas are currently at

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A Mechanism for Decadal Climate Variability,force the initial SST anomaly, so that ocean and atmosphere act as a positive feedback system. The atmospheric response, however, consists also of a wind stress curl anomaly which spins down the subtropical ocean gyre, thereby reducing the poleward heat transport and the initial SST anomaly. The oce

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Analysis of Thermohaline Feedbacks, anomalous differential surface heat flux. The timescale on which the ocean temperature gradient is restored decreases with increasing power, n, in the atmospheric heat transport parameterization. The limits, . = 0, ∞, correspond approximately to the uncoupled cases of fixed surface heat flux and fi

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An Overview of Century Time-Scale Variability in the Climate System: Observations and Models,les. Instead, it is proposed that these fluctuations are linked to interactions within and between the different climate system components. An overview of recent modeling results and the discussion of mechanisms involved show that such interactions internal to the climate system cannot only exhibit