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    The Low-Level Jet as a Western Boundary Current 

    Source: Monthly Weather Review:;1976:;volume( 104 ):;issue: 007:;page 907
    Author(s): Anderson, David L. T.
    Publisher: American Meteorological Society
    Abstract: The low-level jet which flows across the equator and up the Somali coast is considered as a western boundary current of the East African mountain chain. The jet is assumed to be forced by the low-level divergence in the ...
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    Scatterometer Data Interpretation: Measurement Space and Inversion 

    Source: Journal of Atmospheric and Oceanic Technology:;1997:;volume( 014 ):;issue: 006:;page 1298
    Author(s): Stoffelen, Ad; Anderson, David
    Publisher: American Meteorological Society
    Abstract: The geophysical interpretation of the radar measurements from the ERS-1 scatterometer, called σ0, is considered. An important tool in the interpretation of the data is the visualization of the triplets of radar backscatter ...
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    Variational Assimilation of Altimeter Data in a Multilayer Model of the Tropical Pacific Ocean 

    Source: Journal of Physical Oceanography:;1997:;Volume( 027 ):;issue: 005:;page 664
    Author(s): Weaver, Anthony T.; Anderson, David L. T.
    Publisher: American Meteorological Society
    Abstract: A four-dimensional variational method is used to examine the extent to which a time sequence of altimeter measurements can determine the subsurface flow in a linear multilayer model of the tropical Pacific Ocean. The ...
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    Assimilation of Altimeter Data in the ECMWF Ocean Analysis System 3 

    Source: Monthly Weather Review:;2009:;volume( 137 ):;issue: 004:;page 1393
    Author(s): Vidard, Arthur; Balmaseda, Magdalena; Anderson, David
    Publisher: American Meteorological Society
    Abstract: The latest version of the ECMWF ocean analysis system was recently introduced into operational use. This not only provides initial conditions for the monthly and seasonal forecast systems but also creates a historical ...
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    Seasonal Forecasting of Tropical Cyclone Landfall over Mozambique 

    Source: Journal of Climate:;2003:;volume( 016 ):;issue: 023:;page 3932
    Author(s): Vitart, Frédéric; Anderson, David; Stockdale, Tim
    Publisher: American Meteorological Society
    Abstract: The 2000 tropical cyclone season over the South Indian Ocean (SIO) was exceptional in terms of tropical cyclone landfall over Mozambique. Observed data suggest that SIO tropical cyclones have a track significantly more ...
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    Seasonal Transport Variations in the Florida Straits: A Model Study 

    Source: Journal of Physical Oceanography:;1985:;Volume( 015 ):;issue: 006:;page 773
    Author(s): Anderson, David L. T.; Corry, Robert A.
    Publisher: American Meteorological Society
    Abstract: In a previous study Anderson and Corry used a wind-driven two-layer model to study the effects of topography and islands on the seasonal variation of western boundary currents. The work is continued here with topography, ...
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    Initialization of Equatorial Waves in Ocean Models 

    Source: Journal of Physical Oceanography:;1989:;Volume( 019 ):;issue: 001:;page 116
    Author(s): Anderson, David L. T.; Moore, Andrew M.
    Publisher: American Meteorological Society
    Abstract: The relative information content of mass and velocity measurements for initializing low-frequency equatorially trapped waves is considered using analytical arguments and a numerical model For the Kelvin wave, mass and ...
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    Variational Assimilation of XBT Data. Part II. Sensitivity Studies and Use of Smoothing Constraints 

    Source: Journal of Physical Oceanography:;1990:;Volume( 020 ):;issue: 005:;page 689
    Author(s): Sheinbaum, Julio; Anderson, David L. T.
    Publisher: American Meteorological Society
    Abstract: A linear reduced-gravity model of the tropical pacific is used to assimilate XBT data. The model cannot fit the data in the eastern equatorial Pacific for the whole assimilation period. Several experiments with real and ...
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    Variational Assimilation of XBT Data. Part 1 

    Source: Journal of Physical Oceanography:;1990:;Volume( 020 ):;issue: 005:;page 672
    Author(s): Sheinbaum, Julio; Anderson, David L. T.
    Publisher: American Meteorological Society
    Abstract: A variations method based on the adjoint equation technique is used to assimilate data in a relatively simple linear reduced gravity model of the tropical Pacific. Real XBT data are used by identifying the depth of the ...
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    Slowly Propagating Disturbances in a Coupled Ocean-Atmosphere Model 

    Source: Journal of the Atmospheric Sciences:;1985:;Volume( 042 ):;issue: 006:;page 615
    Author(s): Anderson, David L. T.; McCreary, Julian P.
    Publisher: American Meteorological Society
    Abstract: Solutions to a coupled atmosphere model are discussed. The model ocean is a generalization of a reduced-gravity model that includes an equation for the temperature of the layer T. The model atmosphere is linear, baroclinic, ...
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