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    Finite-Time Instabilities of Lower-Stratospheric Flow 

    Source: Journal of the Atmospheric Sciences:;1996:;Volume( 053 ):;issue: 015:;page 2129
    Author(s): Hartmann, D. L.; Palmer, T. N.; Buizza, R.
    Publisher: American Meteorological Society
    Abstract: The linear structures that produce the most in situ energy growth in the lower stratosphere for realistic wintertime flows are investigated using T21 and T42 calculations with the ECMWF 19-level forecast model. Significant ...
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    Singular Vectors: The Effect of Spatial Scale on Linear Growth of Disturbances 

    Source: Journal of the Atmospheric Sciences:;1995:;Volume( 052 ):;issue: 022:;page 3885
    Author(s): Hartmann, D. L.; Buizza, R.; Palmer, T. N.
    Publisher: American Meteorological Society
    Abstract: The scale dependence of rapidly growing perturbations is investigated by studying the dominant singular vectors of T21 and T42 versions of the ECMWF model, which show the most linear energy growth in a 3-day period. A ...
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    Reply 

    Source: Journal of Climate:;2002:;volume( 015 ):;issue: 017:;page 2571
    Author(s): Hartmann, D. L.; Moy, L. A.; Fu, Q.
    Publisher: American Meteorological Society
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    Upper-Tropospheric Water Vapor from UARS MLS 

    Source: Bulletin of the American Meteorological Society:;1995:;volume( 076 ):;issue: 012:;page 2381
    Author(s): Read, W. G.; Waters, J. W.; Flower, D. A.; Froidevaux, L.; Jarnot, R. F.; Hartmann, D. L.; Harwood, R. S.; Rood, R. B.
    Publisher: American Meteorological Society
    Abstract: Initial results of upper-tropospheric water vapor obtained from the Microwave Limb Sounder (MLS) on the Upper Atmosphere Research Satellite (UARS) are presented. MLS is less affected by clouds than infrared or visible ...
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