Geoscience Reference
In-Depth Information
Fig. 6. As shown in Fig. 5, except for rainfall amount (mm) (a) at 18:00 LST, December
7, 2002 and (b) 18:00 LST, December 8.
Fig. 7. As shown in Fig. 5, except for (a) sensible heat flux (W/m
2
) at 18:00 LST,
December 7, 2002 and (b) 18:00 LST, December 8.
by cold ground surface and adiabatic cooling processes during their uprising
toward the mountain top, showing the saturation of transported moisture.
The saturated moisture formed a great low cloud like stratocumulus on the
mountain top and the cloud was observed in the right hand side of the
mountain top under westerly wind in the upwind side of the mountain.
