1. Arizbeth.Olivares

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.

8. Condensation
• Condensation form from whether dew fog or
clouds the air have to be saturated.

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