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    Diagnosis of a Polar Low Warm Core Utilizing the Advanced Microwave Sounding Unit 

    Source: Weather and Forecasting:;2003:;volume( 018 ):;issue: 005:;page 700
    Author(s): Moore, Richard W.; Vonder Haar, Thomas H.
    Publisher: American Meteorological Society
    Abstract: Data from the Advanced Microwave Sounding Unit (AMSU) are used to examine a polar low that occurred in the Labrador Sea on 17?18 March 2000. During its 40-h lifetime, the polar low was observed three times by AMSU, which ...
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    The Modulation of the Subtropical and Extratropical Atmosphere in the Pacific Basin in Response to the Madden–Julian Oscillation 

    Source: Monthly Weather Review:;2010:;volume( 138 ):;issue: 007:;page 2761
    Author(s): Moore, Richard W.; Martius, Olivia; Spengler, Thomas
    Publisher: American Meteorological Society
    Abstract: The 40-yr ECMWF Re-Analysis (ERA-40) data are combined with a number of novel climatologies to conduct a comprehensive examination of the response of the subtropical and extratropical atmosphere over the Pacific basin to ...
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    Reexamining the Dynamics of Short-Scale, Diabatic Rossby Waves and Their Role in Midlatitude Moist Cyclogenesis 

    Source: Journal of the Atmospheric Sciences:;2004:;Volume( 061 ):;issue: 006:;page 754
    Author(s): Moore, Richard W.; Montgomery, Michael T.
    Publisher: American Meteorological Society
    Abstract: As a step toward a more comprehensive study of the physical processes that underlie explosive cyclogenesis, a two-dimensional, semigeostrophic model with a now standard parameterization of latent heat release is used to ...
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    Analysis of an Idealized, Three-Dimensional Diabatic Rossby Vortex: A Coherent Structure of the Moist Baroclinic Atmosphere 

    Source: Journal of the Atmospheric Sciences:;2005:;Volume( 062 ):;issue: 008:;page 2703
    Author(s): Moore, Richard W.; Montgomery, Michael T.
    Publisher: American Meteorological Society
    Abstract: The fifth-generation Pennsylvania State University?National Center for Atmospheric Research (PSU?NCAR) Mesoscale Model (MM5) is used to conduct a number of idealized numerical simulations to confirm recent findings of an ...
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    Interannual Variability of Cloud Forcing and Meridional Energy Transport for the Northern Hemisphere Winter from 1984 to 1990 

    Source: Journal of Climate:;2001:;volume( 014 ):;issue: 017:;page 3643
    Author(s): Moore, Richard W.; Vonder Haar, Thomas H.
    Publisher: American Meteorological Society
    Abstract: Broadband radiative flux data from the Earth Radiation Budget Experiment (ERBE) are used to document the interannual variability of net cloud forcing over the lifetime of the ERBE scanner instruments. The study focuses on ...
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    The Baroclinic Moisture Flux 

    Source: Monthly Weather Review:;2016:;volume( 145 ):;issue: 001:;page 25
    Author(s): McTaggart-Cowan, Ron; Gyakum, John R.; Moore, Richard W.
    Publisher: American Meteorological Society
    Abstract: s subsaturated air ascends sloping isentropic surfaces, adiabatic expansion results in cooling and relative moistening. This process is an effective way to precondition the atmosphere for efficient moist processes while ...
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    The Integral Role of a Diabatic Rossby Vortex in a Heavy Snowfall Event 

    Source: Monthly Weather Review:;2008:;volume( 136 ):;issue: 006:;page 1878
    Author(s): Moore, Richard W.; Montgomery, Michael T.; Davies, Huw C.
    Publisher: American Meteorological Society
    Abstract: On 24?25 February 2005, a significant East Coast cyclone deposited from 4 to nearly 12 in. (?10?30 cm) of snow on parts of the northeastern United States. The heaviest snowfall and most rapid deepening of the cyclone ...
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    Genesis Criteria for Diabatic Rossby Vortices: A Model Study 

    Source: Monthly Weather Review:;2012:;volume( 141 ):;issue: 001:;page 252
    Author(s): Moore, Richard W.; Montgomery, Michael T.; Davies, Huw
    Publisher: American Meteorological Society
    Abstract: suite of idealized mesoscale model simulations are conducted to examine the dynamic pathway to the genesis of short-scale, moist baroclinic disturbances. It is shown that in an initially subsaturated environment, two ...
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    Mesoscale Convective Vortex Formation in a Weakly Sheared Moist Neutral Environment 

    Source: Journal of the Atmospheric Sciences:;2007:;Volume( 064 ):;issue: 005:;page 1443
    Author(s): Conzemius, Robert J.; Moore, Richard W.; Montgomery, Michael T.; Davis, Christopher A.
    Publisher: American Meteorological Society
    Abstract: Idealized simulations of a diabatic Rossby vortex (DRV) in an initially moist neutral baroclinic environment are performed using the fifth-generation National Center for Atmospheric Research?Pennsylvania State University ...
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    A Global Climatology of Baroclinically Influenced Tropical Cyclogenesis 

    Source: Monthly Weather Review:;2012:;volume( 141 ):;issue: 006:;page 1963
    Author(s): McTaggart-Cowan, Ron; Galarneau, Thomas J.; Bosart, Lance F.; Moore, Richard W.; Martius, Olivia
    Publisher: American Meteorological Society
    Abstract: ropical cyclogenesis is generally considered to occur in regions devoid of baroclinic structures; however, an appreciable number of tropical cyclones (TCs) form in baroclinic environments each year. A global climatology ...
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