| 748 |
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 |
| 749 |
to the height of the vegetation elements. |
to the height of the vegetation elements. |
| 750 |
|
|
| 751 |
\paragraph{Gravity Wave Drag}: |
\paragraph{Gravity Wave Drag} |
| 752 |
|
|
| 753 |
The fizhi package employs the gravity wave drag scheme of \cite{zhouetal:95}). |
The fizhi package employs the gravity wave drag scheme of \cite{zhouetal:95}). |
| 754 |
This scheme is a modified version of Vernekar et al. (1992), |
This scheme is a modified version of Vernekar et al. (1992), |
| 833 |
\paragraph{Upper Level Moisture} |
\paragraph{Upper Level Moisture} |
| 834 |
The fizhi package uses climatological water vapor data above 100 mb from the Stratospheric Aerosol and Gas |
The fizhi package uses climatological water vapor data above 100 mb from the Stratospheric Aerosol and Gas |
| 835 |
Experiment (SAGE) as input into the model's radiation packages. The SAGE data is archived |
Experiment (SAGE) as input into the model's radiation packages. The SAGE data is archived |
| 836 |
as monthly zonal means at 5$^\circ$ latitudinal resolution. The data is interpolated to the |
as monthly zonal means at $5^\circ$ latitudinal resolution. The data is interpolated to the |
| 837 |
model's grid location and current time, and blended with the GCM's moisture data. Below 300 mb, |
model's grid location and current time, and blended with the GCM's moisture data. Below 300 mb, |
| 838 |
the model's moisture data is used. Above 100 mb, the SAGE data is used. Between 100 and 300 mb, |
the model's moisture data is used. Above 100 mb, the SAGE data is used. Between 100 and 300 mb, |
| 839 |
a linear interpolation (in pressure) is performed using the data from SAGE and the GCM. |
a linear interpolation (in pressure) is performed using the data from SAGE and the GCM. |