2. http://www.google.com/imgres?q=adiabatic+lifting&hl=en&safe=active&biw=1024&bih=419&gbv=2&tbm=isch&tbnid=_ZLQk
XqmoxH1tM:&imgrefurl=http://www.meted.ucar.edu/fire/s290/unit6/print_2.htm&docid=tpdLN7pCXQIb4M&imgurl=http
://www.meted.ucar.edu/fire/s290/unit6/media/graphics/convergence_ridge.jpg&w=500&h=350&ei=Jk3zTtO1JKnd0QGTld
2CAg&zoom=1&iact=rc&dur=234&sig=100579123846553275600&page=2&tbnh=87&tbnw=137&start=13&ndsp=14&ved=1
t:429,r:1,s:13&tx=38&ty=29
When air is allowed to expand, it cools, and when
it is compressed, it warm
When the temperature changes without adding
hot of cold air it is called adiabatic temperature
changes
When the air is unsaturated and the air warms
up it is called dry adiabatic
When the has water vapor in it the adiabatic rate
is slower then dry adiabatic rate
3. Orographic lifting is when an air mass is
forced from a low elevation to a higher
elevation as it moves over rising terrain.
It is when air is forced to go with the
terrain
http://www.waterencyclopedia.com/Ce-
Cr/Climate-Moderator-Water-as-a.html
http://en.wikipedia.org/wiki/File:Orogra
phic_lifting_of_the_air_-_NOAA.jpg
4. Front
A front is a boundary between a cooling body
mass of hot air and cold air. A frontal wedging is
ware the cold air is in the front
http://www.windows2universe.org/earth/Atmospher
e/tstorm/occl_front.html
http://keithrogershome.com/Chap11Fronts.html
5. Convergence is the natural heating and
culling of the surface. Hot air rises cold air
sinks
Hot air rises because it is less dens
Cold air sinks because it is more dens
http://clem.mscd.edu/~wagnerri/CloudDevel
opment.htm
6. Localized convection is when hot air rises in a
pocket of les dens air and snicks as more dens
cold air
http://en.wikipedia.org/wiki/Convection
7. Stable air stays in its original position, wile
unstable air rises
the most stable conditions for the air is when
air temperature actually increases with
height it Is called a temperature inversion.
http://www.airphotona.com/image.asp?imag
eid=14226&catnum=0&keyword=&country=
&state=&pagenum=556
http://www.targetarea.net/var05.html
8. For condensation to happen the air must be
saturated to make dew, fog, or clouds
When air is saturated the water vapor
condensates on to dust witch is called
condensation nucli.
http://decorating.visitacasas.com/how-to-
combat-condensation/
9. Clouds are classified on the basis of there form and
height.
Cirrus clouds are high White and thin. They can
happen as patches or look like fluffy blankets in
the sky.
Cumulus clouds are single round cloud masses
with a flat base and a appearance that seams
like it is rising.
Stratus clouds are the clouds that cover the sky
completely with small or no brakes in it. With no
individual cloud in it
http://en.wikipedia.org/wiki/File:CirrusField-color.jpg http://www.usatoday.com/weather/wcumulus.htm http://urbanext.illinois.edu/kalani/18.cfm
10. The high clouds are called cirrocumulus cloud
and there are three clouds that make up the
high cloud they are the cirrus, cirrocumulus,
and cirrostratus clouds.
It is 6000m in the air
All high clouds are thin and white and often
made of ice crystals
http://eo.ucar.edu/kids/sky/clouds3.htm
11. The middle clouds also known as the
altocumulus cloud they can change there form in
different conditions
They are 2000, 6000 meters in the air
They can be a Wight or gray with an infrequent
light snow or drizzle mar accompany the clouds
http://www.bigbranch.net/middle%20clouds.htm
12. There is three types of low clouds stratus,
stratocumulus, and nimbostratus.
The stratus cloud is a fog like layer that always cover
the sky. When the cloud gets uneven it becomes an a
stratocumulus cloud
A nimbostratus cloud is the clouds that produce
precipitation
http://ed101.bu.edu/StudentDoc/current/ED101fa10/j
enmks/stratus.html
http://www.tariqweb.com/2011/03/04/stratocumulus-
clouds/
http://en.wikipedia.org/wiki/File:June_2005_dark_clo
ud.jpg
13. Clouds that don’t fit in the three height
categories
The clouds with vertical development are
filed with unstable air and all of them are
related to another.
They can also produce rain
http://www.wbsg.org/weather/weather_clou
ds.asp
14. It starts when the earth cools off rapidly bye
radiation
http://www.scoutingny.com/?m=201008
15. When the temperature is 4c snowflakes
usually melt and continuo as rain drops
When the temperature is -5c ice crystals join
into larger clumps and form a snow flake.
http://www.shutterstock.com/pic-
47930068/stock-vector--glossy-icons-
representing-different-weather-symbol-sun-
clouds-rain-storm-snow-night.html
16. Sleet is the fall of small particles of clear
transparent ice.
Glaze also known as freezing rain it happens
when rain becomes 0c and when it hits a
surface I turns into ice.
Hail is produced in a cumulonimbus cloud it
starts as a small ice pellets that grow by
collecting super cooling water as they fall.
