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    Comments on “Use of Ducting Theory in an Observed Case of Gravity Waves” 

    Source: Journal of the Atmospheric Sciences:;1997:;Volume( 054 ):;issue: 017:;page 2237
    Author(s): Ralph, F. Martin
    Publisher: American Meteorological Society
    Abstract: No abstract available.
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    Reply 

    Source: Journal of the Atmospheric Sciences:;2000:;Volume( 057 ):;issue: 004:;page 599
    Author(s): Ralph, F. Martin
    Publisher: American Meteorological Society
    Abstract: tract
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    Observations of 250-km-Wavelength Clear-Air Eddies and 750-km-Wavelength Mesocyclones Associated with a Synoptic-Scale Midlatitude Cyclone 

    Source: Monthly Weather Review:;1996:;volume( 124 ):;issue: 006:;page 1199
    Author(s): Martin Ralph, F.
    Publisher: American Meteorological Society
    Abstract: Satellite images of a decaying synoptic-scale cyclone over the North Pacific reveal two distinct types of multiple mososcale cyclonic disturbances. The approximate positions of these disturbances within the synoptic-scale ...
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    Using Radar-Measured Radial Vertical Velocities to Distinguish Precipitation Scattering from Clear-Air Scattering 

    Source: Journal of Atmospheric and Oceanic Technology:;1995:;volume( 012 ):;issue: 002:;page 257
    Author(s): Martin Ralph, F.
    Publisher: American Meteorological Society
    Abstract: Thresholds separating regimes for which Rayleigh scattering from precipitation is likely to dominate over Bragg scattering from clear air are established for several common radar wind profiler frequencies. The thresholds ...
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    The Global Distribution of the Time-Average Wind Stress Curl from NSCAT 

    Source: Journal of the Atmospheric Sciences:;2001:;Volume( 058 ):;issue: 002:;page 109
    Author(s): Milliff, Ralph F.; Morzel, Jan
    Publisher: American Meteorological Society
    Abstract: The time-average wind stress curl field for the global ocean is computed from the wind retrievals of the NASA Scatterometer (NSCAT) mission spanning the period 1 October 1996?29 June 1997. Particular attention is paid to ...
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    On the Linkage between Antarctic Surface Water Stratification and Global Deep-Water Temperature 

    Source: Journal of Climate:;2011:;volume( 024 ):;issue: 014:;page 3545
    Author(s): Keeling, Ralph F.; Visbeck, Martin
    Publisher: American Meteorological Society
    Abstract: he suggestion is advanced that the remarkably low static stability of Antarctic surface waters may arise from a feedback loop involving global deep-water temperatures. If deep-water temperatures are too warm, this promotes ...
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    The Influence of Antecedent Atmospheric River Conditions on Extratropical Cyclogenesis 

    Source: Monthly Weather Review:;2021:;volume( 149 ):;issue: 005:;page 1337
    Author(s): Zhang, Zhenhai;Ralph, F. Martin
    Publisher: American Meteorological Society
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    The Existence and Vertical Structure of Fast, Eastward-Moving Disturbances in the Equatorial Troposphere 

    Source: Journal of the Atmospheric Sciences:;1996:;Volume( 053 ):;issue: 004:;page 586
    Author(s): Milliff, Ralph F.; Madden, Roland A.
    Publisher: American Meteorological Society
    Abstract: Eastward phase propagation, at speed faster than 30 m s?1, of a signal in the equatorial troposphere of the Eastern Pacific is detected, first in historical meteorological observations and then in more recent data. A first ...
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    Historical and National Perspectives on Extreme West Coast Precipitation Associated with Atmospheric Rivers during December 2010 

    Source: Bulletin of the American Meteorological Society:;2011:;volume( 093 ):;issue: 006:;page 783
    Author(s): Ralph, F. M.; Dettinger, M. D.
    Publisher: American Meteorological Society
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    Observations of a Mesoscale Ducted Gravity Wave 

    Source: Journal of the Atmospheric Sciences:;1993:;Volume( 050 ):;issue: 019:;page 3277
    Author(s): Ralph, F. M.; Venkateswaran, V.; Crochet, M.
    Publisher: American Meteorological Society
    Abstract: This paper reports coordinated observations of a mesoscale gravity wave made during the FRONTS 84 field experiment conducted in southwestern France in the summer of 1984. The observations were unique in the sense that all ...
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