Cold Front-Cross Section
-
warm air ahead of front is lifted
up and over
- can get intense
showers/thunderstorms at frontal boundary
- Cs and Ci clouds are blown ahead
of the front by upper level winds
- cloud base is generally lower
behind the front.... why???
- further behind the front, the air
is quite dry, few clouds
- steep frontal boundary, slopes
backward into the cold air
- frontal speed averages 15-25 knots
- temperature and wind profiles on
either side of cold front???
- fronts can weaken with time - frontolysis
- fronts can strengthen with time - frontogenesis
- what processes can lead to
frontogenesis?
ANSWER
|
from Meteorology Today by D. Ahrens |
|
Before Passing |
|
While Passing |
|
After Passing |
Winds |
|
south-southwest |
|
gusty; shifting |
|
west-northwest |
Temperature |
|
warm |
|
sudden drop |
|
steadily
dropping |
Pressure |
|
falling
steadily |
|
minimum, then
sharp rise |
|
rising steadily |
Clouds |
|
increasing: Ci,
Cs and Cb |
|
Cb |
|
Cu |
Precipitation |
|
short period of
showers |
|
heavy rains,
sometimes with hail, thunder and lightning |
|
showers then
clearing |
Visibility |
|
fair to poor in
haze |
|
poor, followed
by improving |
|
good, except in
showers |
Dew Point |
|
high; remains
steady |
|
sharp drop |
|
lowering |
|