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    Variations in Near-Global Sea Level Pressure: Another View 

    Source: Journal of Climate:;1988:;volume( 001 ):;issue: 002:;page 225
    Author(s): Barnett, Tim P.
    Publisher: American Meteorological Society
    Abstract: The behavior of large-scale patterns of sea level pressure is documented using a simple composite analysis over the period 1951?85. One interpretation of the maps shows that anomalies of a given sign appear sequentially ...
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    Monte Carlo Climate Forecasting 

    Source: Journal of Climate:;1995:;volume( 008 ):;issue: 005:;page 1005
    Author(s): Barnett, Tim P.
    Publisher: American Meteorological Society
    Abstract: Ensemble forecasts of global climate conditions during the seven largest Pacific warm/cold events of the last 23 years have been made with a new two-tiered climate forecast technique. The internal model variability (IMV) ...
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    The Competition of Freshwater and Radiation in Forcing the Ocean during El Niño 

    Source: Journal of Climate:;1995:;volume( 008 ):;issue: 005:;page 980
    Author(s): Schneider, Niklas; Barnett, Tim P.
    Publisher: American Meteorological Society
    Abstract: The relative roles of heat and freshwater fluxes in forcing the tropical Pacific on interannual timescales are investigated using sophisticated atmospheric and oceanic general circulation models. Interannual density flux ...
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    CORRIGENDUM 

    Source: Journal of Climate:;2000:;volume( 013 ):;issue: 002:;page 511
    Author(s): Barnett, Tim P.; Latif, Mojib
    Publisher: American Meteorological Society
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    Interdecadal Modulation of ENSO Teleconnections 

    Source: Bulletin of the American Meteorological Society:;1998:;volume( 079 ):;issue: 012:;page 2715
    Author(s): Gershunov, Alexander; Barnett, Tim P.
    Publisher: American Meteorological Society
    Abstract: Seasonal climate anomalies over North America exhibit rather large variability between years characterized by the same ENSO phase. This lack of consistency reduces potential statistically based ENSO-related climate ...
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    The Characteristic Spatial and Temporal Scales for SLP, SST, and Air Temperature in the Southern Hemisphere 

    Source: Journal of Applied Meteorology:;1990:;volume( 029 ):;issue: 008:;page 694
    Author(s): Colosi, John; Barnett, Tim P.
    Publisher: American Meteorological Society
    Abstract: This study summarizes results of an analysis of the TOGA drifting buoy observations in the Southern Hemisphere. The data were first quality controlled for gross errors and then screened against climatology and products ...
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    ENSO Influence on Intraseasonal Extreme Rainfall and Temperature Frequencies in the Contiguous United States: Observations and Model Results 

    Source: Journal of Climate:;1998:;volume( 011 ):;issue: 007:;page 1575
    Author(s): Gershunov, Alexander; Barnett, Tim P.
    Publisher: American Meteorological Society
    Abstract: The signature of ENSO in the wintertime frequencies of heavy precipitation and temperature extremes is derived from both observations and atmospheric general circulation model output for the contiguous United States. ENSO ...
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    Reply 

    Source: Journal of Climate:;1999:;volume( 012 ):;issue: 006:;page 1873
    Author(s): Barnett, Tim P.; Latif, Mojib
    Publisher: American Meteorological Society
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    Intercomparison of Two Different Southern Hemisphere Sea Level Pressure Datasets 

    Source: Journal of Climate:;1992:;volume( 005 ):;issue: 001:;page 93
    Author(s): Barnett, Tim P.; Jones, P. D.
    Publisher: American Meteorological Society
    Abstract: Two different sea-level pressure datasets for the strip between 20° and 40°S are intercompared. At large space-time scales the sets are virtually identical. However, for studies of short-term, regional changes caution must ...
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    Numerical Model-Reality Intercomparison Tests Using Small-Sample Statistics 

    Source: Journal of the Atmospheric Sciences:;1983:;Volume( 040 ):;issue: 008:;page 1884
    Author(s): Preisendorfer, Rudolph W.; Barnett, Tim P.
    Publisher: American Meteorological Society
    Abstract: When a numerical model's representation of a physical field is to be compared with a corresponding real observed field, it is usually the case that the numbers of realizations of model and observed field are relatively ...
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