The document discusses various atmospheric and meteorological concepts. It defines dry adiabatic and wet adiabatic rates as how heat changes in unsaturated and saturated air respectively without energy added or subtracted. It also discusses atmospheric stability and instability, frontal wedging caused by cooler air masses sinking below warmer ones, lifting of air causing atmospheric convergence, and the formation of air pockets with lower density surrounded by denser air. Other concepts covered include temperature increases indicating atmospheric stability, fog or dew formation, different types of clouds at high, middle and low levels, and the phases of water from vapor to liquid to solid.

2.  Heat that change if there is not energy add or subtracted from it
 When it is heat or cooling in unsaturated
dry adiabatic rate
 When it is heat or cooling in saturated air it
is called wet adiabatic rate
http://www.richhoffmanclass.com/chapter4.html

3. is like when a mountains act like a stopping point
to get it to go high up
http://ocw.usu.edu/Forest__Range__and_Wildlife_Sciences/Wildland_Fire_Management_and_Planning/Unit_7__Atmospher
ic_Stability_and_Instability_3.html

4.  The process that happen want the cooler
masses goes lower then the hotter masses
http://www.geo.hunter.cuny.edu/~tbw/wc.notes/4.moisture.atm.stability/front
al_wedging.htm

5.  The lifting of the air that make the atmosphere
flow together
https://www.meted.ucar.edu/sign_in.php?go_back_to=http%253A%252F%2
52Fwww.meted.ucar.edu%252Fradar%252Fsevere_signatures%252Fprint
_llconv.htm

6.  Is when air pocket is made and then the
surrounding air make the air pocket less
density
http://rst.gsfc.nasa.gov/Sect14/Sect14_1c.html

7.  The time when air temperature increases
 The most stable time
http://www.epa.gov/AMD/Library/Annual
Reports/2008.html

8.  Is fog or dew
http://www.earthzine.org/2010/06/21/a-
surprising-side-effect-of-climate-change-a-fog-of-
confusion/

9.  Cirrus are high clouds
 Cumulus are middle clouds
 Stratus are low clouds
http://eo.ucar.edu/webweather/cloud3.html

10.  Calledcirrocumulus
 White and thin clouds
 Made up of ice
crystalshttp ://cimss.ssec.wisc.edu/satmet/modules/clouds/highclouds.html

11.  Their calledaltocumulus clouds
 They are larger and denser clouds
 They get us light snow or drizzle
http://ketiltrout.net/ice/gallery.cgi?e=006

12.  There are three part of low clouds are
stratus, stratocumulus and nimbostratus
http://www.instructables.com/id/
Predicting-Weather-with-Clouds/s
tep9/Low-clouds/

13.  Some clouds do not go in the range of
high, middle, and low. They go in the middle of
the range or they are to low to be called low
clouds
http://www.bigbranch.net/cumulus.htm

14.  Fog is not different then a cloud
 Fog is cloud on the ground or right above the
ground
http://www.crh.noaa.gov/jkl/?n=fog_types

15.  This iswant a liquid is at 0 degrees C
 Can freeze a solid object
http://nanopatentsandinnovations.blogspot.com/2010/06/amount-of-
dust-pollen-matters-for-cloud.html

16.  Is when the air fully saturated
http://www.srh.noaa.gov/fwd/?n=warmrainpaper

17.  Snow is rain falling and turn in to snowflakes
 Rain is water that fall from clouds and they
have to be at least 0.5mm big
http://aumusiclibrary.wordpress.com/2011/02/28/rain-helens-picks-for-a-
rainy-afternoon/

18.  Sleet is small particles of clear to translucent ice
 Glaze is the fall as rain drops and turn to ice went
hit the ground
 Hail are small pellets of ice
http://www.erh.noaa.gov/cae/svrwx/hail.htm