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    Comments on “The Fast-Wave Limit and Interannual Oscillations” 

    Source: Journal of the Atmospheric Sciences:;1992:;Volume( 049 ):;issue: 020:;page 1947
    Author(s): Cane, Mark A.
    Publisher: American Meteorological Society
    Abstract: No abstract available.
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    The Near Surface Equatorial Indian Ocean in 1979. Part I: Linear Dynamics 

    Source: Journal of Physical Oceanography:;1984:;Volume( 014 ):;issue: 012:;page 1817
    Author(s): Reverdin, Gilles; Cane, Mark
    Publisher: American Meteorological Society
    Abstract: Different wind field analyses are used to force a one layer adiabatic model of the near equatorial surface circulation in the Indian Ocean in 1979. The model simulates the major features of the observations: eastward jets ...
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    Modeling Sea Level During El Niño 

    Source: Journal of Physical Oceanography:;1984:;Volume( 014 ):;issue: 012:;page 1864
    Author(s): Cane, Mark A.
    Publisher: American Meteorological Society
    Abstract: We test the hypothesis that sea level variations associated with EL Niño events are a response to wind changes in the central Pacific and that the signal is transmitted to the coast of South America by packets of equatorial ...
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    A Mathematical Note on Kawase's Study of the Deep-Ocean Circulation 

    Source: Journal of Physical Oceanography:;1989:;Volume( 019 ):;issue: 004:;page 548
    Author(s): Cane, Mark A.
    Publisher: American Meteorological Society
    Abstract: No abstract available.
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    The Predictability of Tropical Pacific Decadal Variability: Insights from Attractor Reconstruction 

    Source: Journal of the Atmospheric Sciences:;2019:;volume 076:;issue 003:;page 801
    Author(s): Ramesh, Nandini; Cane, Mark A.
    Publisher: American Meteorological Society
    Abstract: AbstractTropical Pacific decadal variability (TPDV), though not the totality of Pacific decadal variability, has wide-ranging climatic impacts. It is currently unclear whether this phenomenon is predictable. In this study, ...
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    A Two-Layer Wind-Driven Ocean Model in a Multiply Connected Domain with Bottom Topography 

    Source: Journal of Physical Oceanography:;1997:;Volume( 027 ):;issue: 011:;page 2395
    Author(s): Krupitsky, Alexander; Cane, Mark A.
    Publisher: American Meteorological Society
    Abstract: The behavior of the solution to a two-layer wind-driven model in a multiply connected domain with bottom topography imitating the Southern Ocean is described. The abyssal layer of the model is forced by interfacial friction, ...
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    Reply 

    Source: Journal of Physical Oceanography:;1999:;Volume( 029 ):;issue: 008:;page 2119
    Author(s): Cane, Mark A.; Kamenkovich, Vladimir
    Publisher: American Meteorological Society
    Abstract: tract
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    Pacific Shallow Meridional Overturning Circulation in a Warming Climate 

    Source: Journal of Climate:;2011:;volume( 024 ):;issue: 024:;page 6424
    Author(s): Wang, Daiwei; Cane, Mark A.
    Publisher: American Meteorological Society
    Abstract: y analyzing a set of the Coupled Model Intercomparison Project phase 3 (CMIP3) climate model projections of the twenty-first century, it is found that the shallow meridional overturning of the Pacific subtropical cells ...
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    Warming Trend of the Indian Ocean SST and Indian Ocean Dipole from 1880 to 2004 

    Source: Journal of Climate:;2008:;volume( 021 ):;issue: 010:;page 2035
    Author(s): Ihara, Chie; Kushnir, Yochanan; Cane, Mark A.
    Publisher: American Meteorological Society
    Abstract: The state of the Indian Ocean dipole representing the SST anomaly difference between the western and southeastern regions of the ocean is investigated using historical SST reconstructions from 1880 to 2004. First, the ...
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    Pacific Decadal Variability in the View of Linear Equatorial Wave Theory 

    Source: Journal of Physical Oceanography:;2009:;Volume( 039 ):;issue: 001:;page 203
    Author(s): Emile-Geay, Julien; Cane, Mark A.
    Publisher: American Meteorological Society
    Abstract: It has recently been proposed, within the framework of the linear shallow-water equations, that tropical Pacific decadal variability (PDV) can be accounted for by basin modes with eigenperiods of 10 to 20 yr, amplifying a ...
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