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    On the Atmospheric Branch of the Hydrological Cycle 

    Source: Journal of Climate:;1993:;volume( 006 ):;issue: 001:;page 161
    Author(s): Chen, Tsing-Chang; Pfaendtner, James
    Publisher: American Meteorological Society
    Abstract: Recently, HIRS2/MSU data have been used at the Goddard Laboratory for Atmospheres(GLA) to generate global precipitation estimates. A synergistic mix of the GLA precipitation, together with the global wind and moisture ...
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    Assimilation Variability in the GEOS-1 Data Assimilation System 

    Source: Monthly Weather Review:;1997:;volume( 125 ):;issue: 004:;page 560
    Author(s): Sienkiewicz, Meta E.; Pfaendtner, James
    Publisher: American Meteorological Society
    Abstract: Ensembles of assimilation runs were used to assess the sensitivity of the GEOS-1 (Goddard Earth Observing System?Version 1) data assimilation system to data gaps and changes in initial conditions. Perturbations from a ...
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    Inclusion of Special Sensor Microwave/imager (SSM/I) Total Precipitable Water Estimates into the GEOS-1 Data Assimilation System 

    Source: Monthly Weather Review:;1995:;volume( 123 ):;issue: 010:;page 3003
    Author(s): Ledvina, David V.; Pfaendtner, James
    Publisher: American Meteorological Society
    Abstract: At this time, most current data assimilation systems use dewpoint depression data, converted to an appropriate moisture variable (relative humidity or mixing ratio), provided by rawinsondes as the lone source of moisture ...
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    A GCM Study on the Maintenance of the June 1982 Blocking in the Southern Hemisphere 

    Source: Journal of the Atmospheric Sciences:;1987:;Volume( 044 ):;issue: 008:;page 1123
    Author(s): Mo, Kingtse C.; Pfaendtner, James; Kalnay, Eugenia
    Publisher: American Meteorological Society
    Abstract: General Circulation Model (GCM) experiments have been performed to determine mechanisms that maintained the blocking episode in the Australian-New Zealand region during the period 8?22 June 1982. A control forecast reproduces ...
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    An Assimilated Dataset for Earth Science Applications 

    Source: Bulletin of the American Meteorological Society:;1993:;volume( 074 ):;issue: 012:;page 2331
    Author(s): Schubert, Siegfried D.; Rood, Richard B.; Pfaendtner, James
    Publisher: American Meteorological Society
    Abstract: The Data Assimilation Office at NASA's Goddard Space Flight Center is currently producing a multiyear gridded global atmospheric dataset for use in climate research, including tropospheric chemistry applications. The data, ...
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    The 12–24-Day Mode of Global Precipitation 

    Source: Monthly Weather Review:;1995:;volume( 123 ):;issue: 001:;page 140
    Author(s): Chen, Tsing-Chang; Chen, Jau-Ming; Pfaendtner, James; Susskind, Joel
    Publisher: American Meteorological Society
    Abstract: Global precipitation estimates derived from satellite data at the Goddard Laboratory for Atmospheres for 1979?80 were used to explore time variations in global precipitation. Time series of the area-averaged precipitation ...
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    The Effect of Horizontal Resolution on Systematic Errors of the GLA Forecast Model 

    Source: Monthly Weather Review:;1990:;volume( 118 ):;issue: 006:;page 1371
    Author(s): Chen, Tsing-Chang; Chen, Jau-Ming; Pfaendtner, James
    Publisher: American Meteorological Society
    Abstract: Systematic prediction errors of the Goddard Laboratory for Atmospheres (GLA) forecast system are reduced when the higher-resolution (2° ? 2.5°) model version is used. Based on a budget analysis of the 200-mb eddy streamfunction, ...
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    Low-Frequency Variations in the Atmospheric Branch of the Global Hydrological Cycle 

    Source: Journal of Climate:;1995:;volume( 008 ):;issue: 001:;page 92
    Author(s): Chen, Tsing-Chang; Chen, Jau-Ming; Pfaendtner, James
    Publisher: American Meteorological Society
    Abstract: According to the atmospheric water balance equation, the divergence of the water vapor flux is responsible for the exchange of water vapor between its source and sink regions. Because the water vapor flux divergence is ...
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