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    A Simple Technique to Infer the Missing Gravity Wave Drag in the Middle Atmosphere Using a General Circulation Model: Potential Vorticity Budget 

    Source: Journal of the Atmospheric Sciences:;2013:;Volume( 071 ):;issue: 002:;page 683
    Author(s): Pulido, Manuel
    Publisher: American Meteorological Society
    Abstract: simple technique to infer the missing momentum forcing in a general circulation model is developed and evaluated. The response of the large-scale dynamic equations to an external momentum forcing presents a nonlocal response ...
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    The Seasonal Cycle of Gravity Wave Drag in the Middle Atmosphere 

    Source: Journal of Climate:;2008:;volume( 021 ):;issue: 018:;page 4664
    Author(s): Pulido, Manuel; Thuburn, John
    Publisher: American Meteorological Society
    Abstract: Using a variational technique, middle atmosphere gravity wave drag (GWD) is estimated from Met Office middle atmosphere analyses for the year 2002. The technique employs an adjoint model of a middle atmosphere dynamical ...
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    Spectral Tail of a Gravity Wave Train Propagating in a Shearing Background 

    Source: Journal of the Atmospheric Sciences:;2000:;Volume( 057 ):;issue: 009:;page 1473
    Author(s): Pulido, Manuel; Caranti, Giorgio
    Publisher: American Meteorological Society
    Abstract: The causes of the appearance of a tail in the power spectrum of a gravity wave train in a shearing background terminating under the Hodges condition are studied. The power spectrum of this train for a wavenumber greater ...
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    Compensation between Resolved and Unresolved Wave Drag in the Stratospheric Final Warmings of the Southern Hemisphere 

    Source: Journal of the Atmospheric Sciences:;2015:;Volume( 072 ):;issue: 011:;page 4393
    Author(s): Scheffler, Guillermo; Pulido, Manuel
    Publisher: American Meteorological Society
    Abstract: he role of planetary wave drag and gravity wave drag in the breakdown of the stratospheric polar vortex and its associated final warming in the Southern Hemisphere is examined using reanalyses from MERRA and a middle-atmosphere ...
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    CORRIGENDUM 

    Source: Journal of Climate:;2009:;volume( 022 ):;issue: 019:;page 5273
    Author(s): Pulido, Manuel; Thuburn, John
    Publisher: American Meteorological Society
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    Parameter Estimation Using Ensemble-Based Data Assimilation in the Presence of Model Error 

    Source: Monthly Weather Review:;2014:;volume( 143 ):;issue: 005:;page 1568
    Author(s): Ruiz, Juan; Pulido, Manuel
    Publisher: American Meteorological Society
    Abstract: his work explores the potential of online parameter estimation as a technique for model error treatment under an imperfect model scenario, in an ensemble-based data assimilation system, using a simple atmospheric general ...
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    A Higher-Order Ray Approximation Applied to Orographic Gravity Waves: Gaussian Beam Approximation 

    Source: Journal of the Atmospheric Sciences:;2010:;Volume( 068 ):;issue: 001:;page 46
    Author(s): Pulido, Manuel; Rodas, Claudio
    Publisher: American Meteorological Society
    Abstract: Ray techniques are a promising tool for developing orographic gravity wave drag schemes. However, the modeling of the propagation of orographic waves using standard ray theory in realistic background wind conditions usually ...
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    Gravity Wave Focusing on the Antarctic Polar Vortex Using Gaussian Beam Approximation in Horizontally Nonuniform Flows 

    Source: Journal of the Atmospheric Sciences:;2021:;volume( 078 ):;issue: 012:;page 3837
    Author(s): Rodas, Claudio;Pulido, Manuel
    Publisher: American Meteorological Society
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    Model Selection: Using Information Measures from Ordinal Symbolic Analysis to Select Model Subgrid-Scale Parameterizations 

    Source: Journal of the Atmospheric Sciences:;2017:;Volume( 074 ):;issue: 010:;page 3253
    Author(s): Pulido, Manuel;Rosso, Osvaldo A.
    Publisher: American Meteorological Society
    Abstract: AbstractThe use of information measures for model selection in geophysical models with subgrid parameterizations is examined. Although the resolved dynamical equations of atmospheric or oceanic global numerical models are ...
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    A Review of Innovation-Based Methods to Jointly Estimate Model and Observation Error Covariance Matrices in Ensemble Data Assimilation 

    Source: Monthly Weather Review:;2020:;volume( 148 ):;issue: 010:;page 3973
    Author(s): Tandeo, Pierre;Ailliot, Pierre;Bocquet, Marc;Carrassi, Alberto;Miyoshi, Takemasa;Pulido, Manuel;Zhen, Yicun
    Publisher: American Meteorological Society
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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
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