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    Comments on “Orographically Forced Planetary Waves in the Northern Hemisphere Winter: Steady State Model with Wave-Coupled Lower Boundary Formulation” 

    Source: Journal of the Atmospheric Sciences:;1988:;Volume( 046 ):;issue: 013:;page 2101
    Author(s): Da Silva, Arlindo M.
    Publisher: American Meteorological Society
    Abstract: We reexamine the coupled lower boundary condition of Chen and Trenberth and show that for consistency the vertical velocity should be corrected from the mountain surface to the lowest computational level. This correction ...
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    A Neural Network Correction to the Scalar Approximation in Radiative Transfer 

    Source: Journal of Atmospheric and Oceanic Technology:;2019:;volume 036:;issue 005:;page 819
    Author(s): Castellanos, Patricia; da Silva, Arlindo
    Publisher: American Meteorological Society
    Abstract: AbstractThe next generation of advanced high-resolution sensors in geostationary orbit will gather detailed information for studying the Earth system. There is an increasing desire to perform observing system simulation ...
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    On the Establishment of Stationary Waves in the Northern Hemisphere Winter 

    Source: Journal of the Atmospheric Sciences:;1993:;Volume( 050 ):;issue: 001:;page 43
    Author(s): Da Silva, Arlindo M.; Lindzen, Richard S.
    Publisher: American Meteorological Society
    Abstract: The establishment of stationary waves in the Northern Hemisphere winter is investigated using stationary and time-dependent linear primitive equation models. Confirming the results of Nigam and Lindzen, we find that small ...
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    A Mechanism for Excitation of Ultralong Rossby Waves 

    Source: Journal of the Atmospheric Sciences:;1987:;Volume( 044 ):;issue: 024:;page 3625
    Author(s): da Silva, Arlindo M.; Lindzen, Richard S.
    Publisher: American Meteorological Society
    Abstract: Ultralong Rossby waves (low zonal and meridional wavenumbers on the sphere) have been studied for many years. Extensive observational evidence tends to identify these waves with the gravest normal modes of the atmosphere. ...
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    Maximum-Likelihood Estimation of Forecast and Observation Error Covariance Parameters. Part I: Methodology 

    Source: Monthly Weather Review:;1999:;volume( 127 ):;issue: 008:;page 1822
    Author(s): Dee, Dick P.; da Silva, Arlindo M.
    Publisher: American Meteorological Society
    Abstract: The maximum-likelihood method for estimating observation and forecast error covariance parameters is described. The method is presented in general terms but with particular emphasis on practical aspects of implementation. ...
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    The Choice of Variable for Atmospheric Moisture Analysis 

    Source: Monthly Weather Review:;2003:;volume( 131 ):;issue: 001:;page 155
    Author(s): Dee, Dick P.; da Silva, Arlindo M.
    Publisher: American Meteorological Society
    Abstract: The implications of using different control variables for the analysis of moisture observations in a global atmospheric data assimilation system are investigated. A moisture analysis based on either mixing ratio or specific ...
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    Using Hough Harmonics to Validate and Assess Nonlinear shallow-Water Models 

    Source: Monthly Weather Review:;1986:;volume( 114 ):;issue: 011:;page 2191
    Author(s): Dee, Dick P.; Da Silva, Arlindo Moraes
    Publisher: American Meteorological Society
    Abstract: The implementation of a technique for locating programming errors in shallow-water codes, establishing the correctness of the code, and assessing the performance of the numerical model under various flow conditions is ...
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    Assimilation of Satellite Cloud Data into the GMAO Finite-Volume Data Assimilation System Using a Parameter Estimation Method. Part I: Motivation and Algorithm Description 

    Source: Journal of the Atmospheric Sciences:;2007:;Volume( 064 ):;issue: 011:;page 3880
    Author(s): Norris, Peter M.; da Silva, Arlindo M.
    Publisher: American Meteorological Society
    Abstract: General circulation models are unable to resolve subgrid-scale moisture variability and associated cloudiness and so must parameterize grid-scale cloud properties. This typically involves various empirical assumptions and ...
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    The Characteristic Rossby Frequency 

    Source: Journal of the Atmospheric Sciences:;1987:;Volume( 044 ):;issue: 007:;page 1100
    Author(s): Straus, David M.; Lindzen, Richard S.; DaSilva, Arlindo Moraes
    Publisher: American Meteorological Society
    Abstract: The characteristic Rossby frequency is defined for a fixed zonal wavenumber perturbation as the variational integral of the Rayleigh-Ritz method. It is a measure of the time scale of the disturbance. For a disturbance which ...
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    Impact of Interactive Aerosol on the African Easterly Jet in the NASA GEOS-5 Global Forecasting System 

    Source: Weather and Forecasting:;2011:;volume( 026 ):;issue: 004:;page 504
    Author(s): Reale, Oreste; Lau, K. M.; da Silva, Arlindo
    Publisher: American Meteorological Society
    Abstract: he real-time treatment of interactive, realistically varying aerosols in a global operational forecasting system, as opposed to prescribed (fixed or climatologically varying) aerosols, is a very difficult challenge that ...
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