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| From: Steve (Primus) (Avatar) |
30/10/2001
5:55:21
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| Subject: re: STEVE'S WEATHER
FAQ |
post id:
476432
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Why does it
get colder in the wee hours. Why is it coldest at dawn?
Radiation from the sun is absorbed by the earth which
warms up. The Earth then radiates in the infra-red range back out into
space. At sunset, the Earth stops getting heated by the sun but continues
to radiate into space. The earth cools down and cools the atmosphere in
contact with it. This cooling continues until the sun comes up again and
starts warming the Earth up. The cross-over point where the incoming
radiation becomes greater than the outgoing radiation is just after
sunrise, so that is the coldest part of the day. In the afternoons, the
crossover point where the outgoing radiation becomes greater than the
incoming radiation is mid to late afternoon - and that is the hottest time
of the day.
The Earth a) emits heat into space and b)
receives heat from the Sun.
If b-a < 0 then the Earth is
cooling. If b-a > 0 then the Earth is heating up. The coldest
time is when the Earth goes from cooling down to heating up. Since b=0
until after dawn, this transition cannot happen until after dawn.
The sun's rays, before it has risen, hitting
the upper atmosphere and warming up way up there.
The
troposphere is mainly heated from below. The warm earth heats the air in
contact with it which, in turn, heats the air above that. Some of the
outgoing longwave radiation from the earth is absorbed by gases in the
troposphere which also adds to the heating. Descending air, such as in the
sub tropical ridge, is heated adiabatically by being compressed as it
descends. Heat in the upper atmosphere has little if any effect on the
surface.
Please remind me what adiabitic means?
Adiabatic processes presume that changes in
temperature, pressure and density within a parcel of air are caused by
changes in altitude without losing energy to the outside or gaining energy
from it. In real life, of course, this does not happen but it makes a
useful model for describing atmospheric
processes.
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