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    On the Physical Mechanism of the Inflection Point Instability 

    Source: Journal of the Atmospheric Sciences:;1972:;Volume( 029 ):;issue: 005:;page 984
    Author(s): Brown, Robert A.
    Publisher: American Meteorological Society
    Abstract: No abstract available.
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    A Gradient Wind Correction for Surface Pressure Fields Retrieved from Scatterometer Winds 

    Source: Journal of Applied Meteorology:;2002:;volume( 041 ):;issue: 002:;page 133
    Author(s): Patoux, Jérôme; Brown, Robert A.
    Publisher: American Meteorological Society
    Abstract: Given a field of geostrophic winds and at least one pressure observation, a pressure field can be computed. If the winds are in reality gradient winds, then a correction must be applied to calculate the actual geostrophic ...
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    Southern Hemisphere Synoptic Weather from a Satellite Scatterometer 

    Source: Monthly Weather Review:;1990:;volume( 119 ):;issue: 012:;page 2803
    Author(s): Levy, Gad; Brown, Robert A.
    Publisher: American Meteorological Society
    Abstract: Analyses of remotely sensed wind vector data from six satellite passes over parts of the Southern Ocean during September 1978 are shown. Winds are input to a planetary boundary layer model to produce sea level pressure ...
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    Ocean Surface Pressure Fields from Satellite-Sensed Winds 

    Source: Monthly Weather Review:;1986:;volume( 114 ):;issue: 011:;page 2197
    Author(s): Brown, Robert A.; Levy, Gad
    Publisher: American Meteorological Society
    Abstract: The University of Washington's planetary boundary layer model is inverted to use remotely sensed satellite scatterometer-derived surface winds as input to calculate maritime surface pressure fields. The analysis of three ...
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    Scatterometer Observations at High Wind Speeds 

    Source: Journal of Applied Meteorology:;1998:;volume( 037 ):;issue: 011:;page 1412
    Author(s): Zeng, Lixin; Brown, Robert A.
    Publisher: American Meteorological Society
    Abstract: Satellite scatterometer winds are commonly validated by comparing them to buoy observations and/or numerical model surface wind analyses. However, the empirical scatterometer algorithm (geophysical model function) has been ...
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    Comparison of Planetary Boundary Layer Model Winds with Dropsonde Observations in Tropical Cyclones 

    Source: Journal of Applied Meteorology:;2001:;volume( 040 ):;issue: 010:;page 1718
    Author(s): Brown, Robert A.; Zeng, Lixin
    Publisher: American Meteorological Society
    Abstract: The values of surface winds simulated by the University of Washington (UW) two-layer similarity planetary boundary layer (PBL) model are compared with National Oceanic and Atmospheric Administration Hurricane Research ...
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    Multiscale Large Eddy States in Weakly Stratified Planetary Boundary Layers 

    Source: Journal of the Atmospheric Sciences:;1989:;Volume( 047 ):;issue: 004:;page 414
    Author(s): Mourad, Pierre D.; Brown, Robert A.
    Publisher: American Meteorological Society
    Abstract: We first discuss observations of two classes of two-dimensional large eddy states in weakly stratified atmospheric boundary layers. One class is characterized by large eddies with a single horizontal scale. The other ...
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    Legacy of the Seasat Mission for Studies of the Atmosphere and Air-Sea-Ice Interactions 

    Source: Bulletin of the American Meteorological Society:;1991:;volume( 072 ):;issue: 007:;page 967
    Author(s): Katsaros, Kristina B.; Brown, Robert A.
    Publisher: American Meteorological Society
    Abstract: The polar-orbiting satellite, Seasat, had been designed as an oceanographic satellite with little advance thought being given to atmospheric uses. However, the microwave instruments provided a rich source of data for ...
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    An Evaluation of Scatterometer-Derived Oceanic Surface Pressure Fields 

    Source: Journal of Applied Meteorology and Climatology:;2008:;volume( 047 ):;issue: 003:;page 835
    Author(s): Patoux, Jérôme; Foster, Ralph C.; Brown, Robert A.
    Publisher: American Meteorological Society
    Abstract: Oceanic surface pressure fields are derived from the NASA Quick Scatterometer (QuikSCAT) surface wind vector measurements using a two-layer similarity planetary boundary layer model in the midlatitudes and a mixed layer ...
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    Diagnosis of Frontal Instabilities over the Southern Ocean 

    Source: Monthly Weather Review:;2005:;volume( 133 ):;issue: 004:;page 863
    Author(s): Patoux, Jérôme; Hakim, Gregory J.; Brown, Robert A.
    Publisher: American Meteorological Society
    Abstract: The development of three fronts over the Southern Ocean is described using SeaWinds-on-QuikSCAT scatterometer surface winds and an attribution technique to partition the wind field in three components: nondivergent and ...
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