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    Is a Cold Pool Necessary for the Maintenance of a Squall Line Produced by a Cold Front Aloft? 

    Source: Monthly Weather Review:;2003:;volume( 131 ):;issue: 001:;page 95
    Author(s): Stoelinga, Mark T.; Locatelli, John D.; Schwartz, Ralph D.; Hobbs, Peter V.
    Publisher: American Meteorological Society
    Abstract: On 19?20 June 1979 a cyclone moved through the central United States. This cyclone contained a squall line associated with a cold front aloft (CFA), which caused significant damage. The fifth-generation Pennsylvania State ...
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    Surface Convergence Induced by Cold Fronts Aloft and Prefrontal Surges 

    Source: Monthly Weather Review:;1997:;volume( 125 ):;issue: 011:;page 2808
    Author(s): Locatelli, John D.; Stoelinga, Mark T.; Schwartz, Ralph D.; Hobbs, Peter V.
    Publisher: American Meteorological Society
    Abstract: The magnitude of surface convergence, produced by the movement of cold fronts aloft and prefrontal surges, is derived by applying the linear divergence equation to observed surface pressure traces for Pacific Northwest ...
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    Norwegian-Type and Cold Front Aloft–Type Cyclones East of the Rocky Mountains 

    Source: Weather and Forecasting:;2002:;volume( 017 ):;issue: 001:;page 66
    Author(s): Locatelli, John D.; Schwartz, Ralph D.; Stoelinga, Mark T.; Hobbs, Peter V.
    Publisher: American Meteorological Society
    Abstract: Conventional data and mesoscale model simulations are used to analyze two cyclones that developed east of the Rocky Mountains in June and November 1998. Both cyclones formed when a Pacific cold front overtook a lee ...
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    CORRIGENDUM 

    Source: Monthly Weather Review:;2003:;volume( 131 ):;issue: 004:;page 744
    Author(s): Stoelinga, Mark T.; Locatelli, John D.; Schwartz, Ralph D.; Hobbs, Peter V.
    Publisher: American Meteorological Society
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