2. Abiotic
Temperature Changes and Expansion
and Cooling
Adiabatic is the temperature that happens
eve though that heat isn’t added or
subtracted.
The rate of adiabatic cooling or heating in
saturated air is called the dry adiabatic rate
http://10.85.0.4:8080/ibreports/ibp/bp.html?f
n=Students&fp=1&ip=10.182.1.26&ibip=10.85.
0.4&ldu=0&re=0&bu=users.tpg.com.au/users/
rwest000/mangrove/abiotic.html&bc=Website
%20contains%20prohibited%20Mobile%20Pho
nes%20content.
3. Or graphic Lifting
• Most of the time it happens while the
elevated terrains such as mountains, Act as
barriers to air flow ,forcing the air to ascend
http://www.waterencyclopedia.com/Ce-
Cr/Climate-Moderator-Water-as-a.html
4. Frontal Wedging
• Is the boundary between cooling masses of
warm and cold air. Frontal wedging is a
process that accurse at a front in witch cold
denses air acts as a barrier over which warmer
less denses air rise.
http://highdefinitionwallpapers.org/wallpaper-
frontal-wedging
5. Convergence
• Lifting of air that results from air in lower
atmosphere flooding together.
http://riverdaughter.wordpress.com/2011/05/
28/convergence-reckless-endangerment-and-
can-you-afford-to-retire/
6. Localized Convective
• Occurs when unequal heating of Earth’s
surface warms a pocket of air more than the
surrounding air, lowering the air pocket’s
density.
http://eo.ucar.edu/kids/dangerwx/tstorm4.ht
m
7. Stability (Densit Diffrerences
&
Stability and Daily Weather)
• con diction that happens when the air
temperature actually increase with, height
called a temperature inversion.
9. Types of clouds
• they are classified on the basis of their
form and height
• Cl0ouds that are white, and thin. They
can accour as patches or as delicate vial-
like sheets or extended wispy fiber that
often have a feathery appearance.
10. High clouds
• Are usually ranging from about 16,5000 and
5,4000ft in latitude
11. Middle clouds
• Appear in the middle range from about 2000
to 6000 meter have the prefix alto as part of
their name
12. Low clouds
• Three members of the family low clouds they
are stratus, stratocumulus, and nimbostratus
13. Clouds of Vertical Development
• Clouds that don’t fit in the one of the three
height categories mentioned.
14. Fog
When cool air moves over warm
water, enough moisture may evaporate from
the water surface to produce saturation
The rising of the water vapor meets the cool
air it immediately condenses and rises with
the air that is being warmer from below
http://es.wikipedia.org/wiki/Archivo:Dense_Se
attle_Fog.jpg
15. Cold clouds precipitation
(Bergergo process)
• The process is a theory that relates the
formation of precipitation to super cooled
clouds, freezing nuclei, and the different
saturation levels of ice and liquid
•
http://www.google.com.do/imgres?q=Cold+clouds+precip
itation&um=1&hl=es&safe=active&biw=1024&bih=419&t
bm=isch&tbnid=LN-
uDK235EHKJM:&imgrefurl=http://nanopatentsandinnovat
ions.blogspot.com/2010/06/amount-of-dust-pollen-
matters-for-cloud.html&docid=a3ZcEv
16. Warm cloud precipitation
• When air is saturated (100% relative
humidity) http://web.me.com/uriarte/Earths
_Climate/16._Other_phenomena.h
tml
17. Sleet glaze and hail
• Facts
• Sleet-small particles of clear to translucent
• Glaze – also knew as freezingg rain happens
when super cooled raind droops
• Hail – produce cumulonimbus cloud hailstones
are small ice pellets but they get largers they
collect super cooled watercooled.
http://www.alabamawx.com/?tag=sleet
