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    A Simple Model of the Atmospheric Response to ENSO Sea Surface Temperature Anomalies 

    Source: Journal of the Atmospheric Sciences:;1991:;Volume( 048 ):;issue: 001:;page 3
    Author(s): Kleeman, R.
    Publisher: American Meteorological Society
    Abstract: A low-order tropical atmospheric model is developed that gives a reasonable account of the tropical precipitation and circulation anomalies observed during various El Niño and La Niña events. The dynamical part of the model ...
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    Multiple Equilibria in a Global Ocean General Circulation Model 

    Source: Journal of Physical Oceanography:;1993:;Volume( 023 ):;issue: 008:;page 1670
    Author(s): Power, S. B.; Kleeman, R.
    Publisher: American Meteorological Society
    Abstract: A global ocean general circulation model is forced using various upper boundary conditions (BCs) on temperature and salinity. Solutions are obtained under restoring and mixed BCs (i.e., a restoring condition on the upper-level ...
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    Greenhouse Warming, Decadal Variability, or El Niño? An Attempt to Understand the Anomalous 1990s 

    Source: Journal of Climate:;1997:;volume( 010 ):;issue: 009:;page 2221
    Author(s): Latif, M.; Kleeman, R.; Eckert, C.
    Publisher: American Meteorological Society
    Abstract: The dominant variability modes in the Tropics are investigated and contrasted with the anomalous situation observed during the last few years. The prime quantity analyzed is anomalous sea surface temperature (SST) in the ...
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    The Linear Response of ENSO to the Madden–Julian Oscillation 

    Source: Journal of Climate:;2005:;volume( 018 ):;issue: 013:;page 2441
    Author(s): Zavala-Garay, J.; Zhang, C.; Moore, A. M.; Kleeman, R.
    Publisher: American Meteorological Society
    Abstract: The possibility that the tropical Pacific coupled system linearly amplifies perturbations produced by the Madden?Julian oscillation (MJO) is explored. This requires an estimate of the low-frequency tail of the MJO. Using ...
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    Modeling the Surface Heat Flux Response to Long-Lived SST Anomalies in the North Atlantic 

    Source: Journal of Climate:;1995:;volume( 008 ):;issue: 009:;page 2161
    Author(s): Power, S. B.; Kleeman, R.; Colman, R. A.; McAvaney, B. J.
    Publisher: American Meteorological Society
    Abstract: An atmospheric general circulation model (AGCM), a simplified atmospheric model (SAM) of surface heat flux, and various idealized analytic models have been used to investigate the atmospheric response over the North Atlantic ...
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    The Response of a Coupled Model of ENSO to Observed Estimates of Stochastic Forcing 

    Source: Journal of Climate:;2003:;volume( 016 ):;issue: 017:;page 2827
    Author(s): Zavala-Garay, J.; Moore, A. M.; Perez, C. L.; Kleeman, R.
    Publisher: American Meteorological Society
    Abstract: In this work the role that observed intraseasonal atmospheric variability may play in controlling and maintaining ENSO variability is examined. To this end, an asymptotically stable intermediate coupled model of El ...
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    Sensitivity of Hybrid ENSO Models to Unresolved Atmospheric Variability 

    Source: Journal of Climate:;2008:;volume( 021 ):;issue: 015:;page 3704
    Author(s): Zavala-Garay, J.; Zhang, C.; Moore, A. M.; Wittenberg, A. T.; Harrison, M. J.; Rosati, A.; Vialard, Jérôme; Kleeman, R.
    Publisher: American Meteorological Society
    Abstract: A common practice in the design of forecast models for ENSO is to couple ocean general circulation models to simple atmospheric models. Therefore, by construction these models (known as hybrid ENSO models) do not resolve ...
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