/[MITgcm]/manual/s_phys_pkgs/text/fizhi.tex
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revision 1.11 by molod, Tue Aug 2 15:50:51 2005 UTC revision 1.12 by molod, Tue Aug 2 21:17:38 2005 UTC
# Line 360  Band & Spectral Range (cm$^{-1}$) & Abso Line 360  Band & Spectral Range (cm$^{-1}$) & Abso
360  \end{tabular}  \end{tabular}
361  \end{center}  \end{center}
362  \vspace{0.1in}  \vspace{0.1in}
363  \caption{IR Spectral Bands, Absorbers, and Parameterization Method (from \cite{chzs:94})}  \caption{IR Spectral Bands, Absorbers, and Parameterization Method (from \cite{chsz:94})}
364  \label{tab:fizhi:longwave}  \label{tab:fizhi:longwave}
365  \end{table}  \end{table}
366    
# Line 431  The cloud fraction values are time-avera Line 431  The cloud fraction values are time-avera
431  hours).  Therefore, in a time-averaged sense, both convective and large-scale  hours).  Therefore, in a time-averaged sense, both convective and large-scale
432  cloudiness can exist in a given grid-box.    cloudiness can exist in a given grid-box.  
433    
434  Turbulence:  \paragraph{Turbulence}:
435    
436  Turbulence is parameterized in the fizhi package to account for its contribution to the  Turbulence is parameterized in the fizhi package to account for its contribution to the
437  vertical exchange of heat, moisture, and momentum.    vertical exchange of heat, moisture, and momentum.  
# Line 754  sun), the greenness fraction, the vegeta Line 754  sun), the greenness fraction, the vegeta
754  Modifications are made to account for the presence of snow, and its depth relative  Modifications are made to account for the presence of snow, and its depth relative
755  to the height of the vegetation elements.  to the height of the vegetation elements.
756    
757  Gravity Wave Drag:  \paragraph{Gravity Wave Drag}:
758    
759  The fizhi package employs the gravity wave drag scheme of \cite{zhouetal:96}).  The fizhi package employs the gravity wave drag scheme of \cite{zhouetal:95}).
760  This scheme is a modified version of Vernekar et al. (1992),  This scheme is a modified version of Vernekar et al. (1992),
761  which was based on Alpert et al. (1988) and Helfand et al. (1987).    which was based on Alpert et al. (1988) and Helfand et al. (1987).  
762  In this version, the gravity wave stress at the surface is  In this version, the gravity wave stress at the surface is
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