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    Temporal and Spatial Interpolation Errors of High-Resolution Modeled Atmospheric Fields 

    Source: Journal of Atmospheric and Oceanic Technology:;2015:;volume( 033 ):;issue: 002:;page 303
    Author(s): Privé, N. C.; Errico, R. M.
    Publisher: American Meteorological Society
    Abstract: eneral circulation models can now be run at very high spatial resolutions to capture finescale features, but saving the full-spatial-resolution output at every model time step is usually not practical because of storage ...
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    The Behavior of Gravitational Modes in Numerical Forecasts with the NCAR Community Climate Model 

    Source: Monthly Weather Review:;1988:;volume( 116 ):;issue: 009:;page 1737
    Author(s): Errico, R. M.; Williamson, D. L.
    Publisher: American Meteorological Society
    Abstract: Characteristics of gravitational-wave noise in noninitialized forecasts were investigated with the NCAR Community Climate Model. Forecasts were begun from FGGE analyses. The behavior of individual, gravitational normal ...
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    Uncertainty of Observation Impact Estimation in an Adjoint Model Investigated with an Observing System Simulation Experiment 

    Source: Monthly Weather Review:;2019:;volume 147:;issue 009:;page 3191
    Author(s): Privé, N. C.; Errico, R. M.
    Publisher: American Meteorological Society
    Abstract: AbstractAdjoint models are often used to estimate the impact of different observations on short-term forecast skill. A common difficulty with the evaluation of short-term forecast quality is the choice of verification ...
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    The Impact of Increased Frequency of Rawinsonde Observations on Forecast Skill Investigated with an Observing System Simulation Experiment 

    Source: Monthly Weather Review:;2014:;volume( 142 ):;issue: 005:;page 1823
    Author(s): Privé, N. C.; Errico, R. M.; Tai, K.-S.
    Publisher: American Meteorological Society
    Abstract: ost rawinsondes are launched once or twice daily, at 0000 and/or 1200 UTC; only a small number of the total rawinsonde observations are taken at 0600 and 1800 UTC (?off hour? cycle times). In this study, the variations of ...
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