Geoscience Reference
In-Depth Information
Fig. 9. (a) Vertical profiles of total cloud mixing ratio (g/kg). (b) relative humidity
(%), (c) rainfall amount (mm) and (d) sensible heat flux (W/m
2
)at10mheightover
the ground surface, respectively.
Even if north-westerly wind coming from northern China made air
parcels be cooled down, generally air parcels with a small amount of mois-
ture in winter could not be saturated, resulting in no existence of snowfall
in the coastal region.
3.3.
Comparison of precipitation and snowfall
Through 78 h numerical simulation with NCEP data sets, numerical simula-
tion results of winter rainfall amounts were compared with precipitation and
