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    Simulated Changes in Storm Morphology Associated with a Sea-Breeze Air Mass 

    Source: Monthly Weather Review:;2021:;volume( 149 ):;issue: 002:;page 333
    Author(s): Hartigan, Joshua;Warren, Robert A.;Soderholm, Joshua S.;Richter, Harald
    Publisher: American Meteorological Society
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    An Improved Instability–Shear Hail Proxy for Australia 

    Source: Monthly Weather Review:;2023:;volume( 151 ):;issue: 002:;page 545
    Author(s): Raupach, Timothy H.; Soderholm, Joshua; Protat, Alain; Sherwood, Steven C.
    Publisher: American Meteorological Society
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    A Radar-Based Hail Climatology of Australia 

    Source: Monthly Weather Review:;2024:;volume( 152 ):;issue: 002:;page 607
    Author(s): Brook, Jordan P.; Soderholm, Joshua S.; Protat, Alain; McGowan, Hamish; Warren, Robert A.
    Publisher: American Meteorological Society
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    HailTrack—Improving Radar-Based Hailfall Estimates by Modeling Hail Trajectories 

    Source: Journal of Applied Meteorology and Climatology:;2021:;volume( 060 ):;issue: 003:;page 237
    Author(s): Brook, Jordan P.;Protat, Alain;Soderholm, Joshua;Carlin, Jacob T.;McGowan, Hamish;Warren, Robert A.
    Publisher: American Meteorological Society
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    The Coastal Convective Interactions Experiment (CCIE): Understanding the Role of Sea Breezes for Hailstorm Hotspots in Eastern Australia 

    Source: Bulletin of the American Meteorological Society:;2015:;volume( 097 ):;issue: 009:;page 1687
    Author(s): Soderholm, Joshua; McGowan, Hamish; Richter, Harald; Walsh, Kevin; Weckwerth, Tammy; Coleman, Matthew
    Publisher: American Meteorological Society
    Abstract: hunderstorm-affected communities develop an awareness of ?hotspot? regions that historically experience more frequent or intense storm activity across many years. A scientifically based understanding of this localized ...
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    Linear Rainfall Features and Their Association with Rainfall Extremes near Melbourne, Australia 

    Source: Monthly Weather Review:;2021:;volume( 149 ):;issue: 010:;page 3401
    Author(s): Hitchcock, Stacey M.;Lane, Todd P.;Warren, Robert A.;Soderholm, Joshua S.
    Publisher: American Meteorological Society
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    An Improved Instability–Shear Hail Proxy for Australia 

    Source: Monthly Weather Review:;2023:;volume( 151 ):;issue: 002
    Author(s): Raupach, Timothy H.; Soderholm, Joshua; Protat, Alain; Sherwood, Steven C.
    Publisher: American Meteorological Society
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    Fostering Science–Industry Connections in Australia’s Severe Storm Science Community 

    Source: Bulletin of the American Meteorological Society:;2024:;volume( 105 ):;issue: 003:;page E559
    Author(s): Raupach, Timothy H.; Soderholm, Joshua S.; Aldridge, Joanna
    Publisher: American Meteorological Society
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    Diurnal Preconditioning of Subtropical Coastal Convective Storm Environments 

    Source: Monthly Weather Review:;2017:;volume( 145 ):;issue: 009:;page 3839
    Author(s): Soderholm, Joshua S.;McGowan, Hamish A.;Richter, Harald;Walsh, Kevin;Wedd, Tony;Weckwerth, Tammy M.;AbstractBoundary layer evolution in response to diurnal forcing is manifested at the mesobeta and smaller scales of the atmosphere. Because this variability resides on subsynoptic scales, the potential influence upon convective storm environments is often not captured in coarse observational and modeling datasets, particularly for complex physical settings such as coastal regions. A detailed observational analysis of diurnally forced preconditioning for convective storm environments of South East Queensland, Australia (SEQ), during the Coastal Convective Interactions Experiment (2013?15) is presented. The observations used include surface-based measurements, aerological soundings, and dual-polarization Doppler radar. The sea-breeze circulation was found to be the dominant influence; however, profile modification by the coastward advection of the continental boundary layer was found to be an essential mechanism for favorable preconditioning of deep convection. This includes 1) enhanced moisture in the city of Brisbane, potentiality due to an urban heat island?enhanced land?sea thermal contrast, 2) significant afternoon warming and moistening above the sea breeze resulting from the advection of the inland convective boundary layer coastward under prevailing westerly flow coupled with the sea-breeze return flow, and 3) substantial variations in near-surface moisture likely associated with topography and land use. For the 27 November 2014 Brisbane hailstorm, which caused damages exceeding $1.5 billion Australian dollars (AUD), the three introduced diurnal preconditioning processes are shown to favor a mesoscale convective environment supportive of large hailstone growth. The hybrid high-precipitation supercell storm mode noted for this event and previous similar events in SEQ is hypothesized to be more sensitive to variations in near-surface and boundary layer instability in contrast to contemporary supercell storms.
    Publisher: American Meteorological Society
    Abstract: AbstractBoundary layer evolution in response to diurnal forcing is manifested at the mesobeta and smaller scales of the atmosphere. Because this variability resides on subsynoptic scales, the potential influence upon ...
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