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    EDITORIAL 

    Source: Journal of Applied Meteorology:;2000:;volume( 039 ):;issue: 011:;page 1809
    Author(s): Garstang, Michael
    Publisher: American Meteorological Society
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    A Review of the Tropical Boundary Layer and Cumulus Convection: Structure, Parameterization, and Modeling 

    Source: Bulletin of the American Meteorological Society:;1974:;volume( 055 ):;issue: 010:;page 1195
    Author(s): Garstang, Michael; Betts, Alan K.
    Publisher: American Meteorological Society
    Abstract: Recent advances in our understanding of the boundary layer and cumulus convection in the tropics are reviewed. The review reflects the interactive nature of the atmosphere-ocean system. It discusses the observational picture ...
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    Vertical Structure of the Tropical Boundary Layer 

    Source: Monthly Weather Review:;1981:;volume( 109 ):;issue: 007:;page 1512
    Author(s): Fitzjarrald, Dayid R.; Garstang, Michael
    Publisher: American Meteorological Society
    Abstract: Obsemations presented show that the undisturbed subcloud layer near the ITCZ resembles that of the trades. Mixed and transition layers are also seen between cloud drafts during disturbed periods when shallow mixed layers ...
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    The Joanne Simpson Special Issue on the Tropical Rainfall Measuring Mission (TRMM) 

    Source: Journal of Applied Meteorology:;2000:;volume( 039 ):;issue: 012:;page 1961
    Author(s): Garstang, Michael; Kummerow, Christian D.
    Publisher: American Meteorological Society
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    Boundary-Layer Growth over the Tropical Ocean 

    Source: Monthly Weather Review:;1981:;volume( 109 ):;issue: 008:;page 1762
    Author(s): Fitzjarrald, David R.; Garstang, Michael
    Publisher: American Meteorological Society
    Abstract: Results of a one-dimensional mixed-layer growth model are compared with thermodynamic observations made during the GARP Atlantic Tropical Experiment (GATE). Observed drying at low levels accompanying warming in the wake ...
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    Subcloud Layer Energetics of Precipitating Convection 

    Source: Monthly Weather Review:;1982:;volume( 110 ):;issue: 002:;page 102
    Author(s): Barnes, Gary M.; Garstang, Michael
    Publisher: American Meteorological Society
    Abstract: The thermodynamic modification of the subcloud layer in the GATE area is shown to be a function of precipitating convection. A critical rate of 2 mm h?1, based on the Z ? R relationship, in conjunction with 4 km ? 4 km ...
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    The Role of Surface Divergence and Vorticity in the Life Cycle of Convective Rainfall. Part I: Observation and Analysis 

    Source: Journal of the Atmospheric Sciences:;1978:;Volume( 035 ):;issue: 006:;page 1047
    Author(s): Ulanski, Stanley L.; Garstang, Michael
    Publisher: American Meteorological Society
    Abstract: The role of the surface velocity fields in the formation, maintenance and decay of convective storms is examined using approximately 90 days of measurements in a densely instrumented network (660 km2) in south Florida. The ...
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    The Role of Surface Divergence and Vorticity in the Life Cycle of Convective Rainfall. Part II: Descriptive Model 

    Source: Journal of the Atmospheric Sciences:;1978:;Volume( 035 ):;issue: 006:;page 1063
    Author(s): Ulanski, Stanley L.; Garstang, Michael
    Publisher: American Meteorological Society
    Abstract: Three stages, prerain, mature and decay, in the life cycle of a convective storm are shown by compiling surface observations from 12 well-organized Florida summertime thunderstorms. In the mature stage, a distinction is ...
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    A Study of a Non-Deepening Tropical Disturbance 

    Source: Journal of Applied Meteorology:;1967:;volume( 006 ):;issue: 002:;page 237
    Author(s): Simpson, Joanne; Garstang, Michael; Zipser, Edward J.; Dean, Gordon A.
    Publisher: American Meteorological Society
    Abstract: Data for a 3-day period from an experimental region formed by 6 islands of the Windward Group in the West Indies, a research vessel in the tropical Atlantic, an instrumented aircraft, and TIROS VI and VII form the basis ...
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    The Daily Cycle of Low-Frequency Elephant Calls and Near-Surface Atmospheric Conditions 

    Source: Earth Interactions:;2005:;volume( 009 ):;issue: 014:;page 1
    Author(s): Garstang, Michael; Fitzjarrald, David R.; Fristrup, Kurt; Brain, Conrad
    Publisher: American Meteorological Society
    Abstract: Elephant low-frequency calls and atmospheric conditions that influence the transmission and detection of these calls were recorded at a fixed location over a period of about 3 weeks at the end of the dry season in the ...
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