5jcastillo
TRANSCRIPT
CLOUDS AND THERE ACQUAINTANCES
By Jacob Castillo
http://www.maestronews.com/wallpaper/clouds/16920.html
Adiabatic Temperature Changes and Expansion and cooling
Temp changes that happen without heat As you travel upward gas expands and
temp gets cooler and cooler as you go The dry adiabatic rate is for every 1000
feet ascending temp goes down 10 degrees celcius
The wet rate is 5-9 degrees celcius per 1000 meters
http://www.kidsgeo.com/geography-for-kids/0070-adiabatic-temperature-changes.php
Orographic Lifting
As you go up a mountain slope adiabatic cooling happens creating clouds and precipitation,
This process only occurs because of the mountain or elevated terrain act as walls or barriers
press&siever12.3.png
Frontal Wedging
When a cold front meets a warm front and the cooler and denser cold front air acts as a wall over when the warmer less dense air rises
frontal.wedging.jpg
Convergence
When converging wind meet each other and because they cannot go down, they go up
circulation‑low2.gif
Localized convective lifting
Unequal heating of the earth causes spots of air in the atmosphere to be more heated than the surrounding air
The spots are called thermals
lift_frontal.jpg
Stability
Air that resists vertical movement Is measured by measuring the earth’s
atmospheric temperature at different heights
Air is stable when the temp goes down a little bit with an increase in altitude
Stable air resists vertical movement Clouds with unstable air often generates
thunderstormshttp://www.google.com/imgres?q=thunderstorms=1t:429,r:8,s:0
Condensation
Condensation happens when water vapor in the air changes to a liquid
For condensation to happen the air must be saturated and there must be a surface
http://www.google.com/imgres?q=dew&hl=en&safe=active&gbv=2&biw=1024&bih=429&tbm=isch&tbnid=jKms9pu1yBhy8M:&imgrefurl=http://www.engr.psu.edu/j
Types of clouds
Clouds are classified based on there form and altitude
There are three types of clouds called the: cirrus, cumulus and the stratus
The cirrus clouds are very high white and thin Cumulus clouds have a flat base with a dome
over it Stratus Clouds are Sheets or layers that cover
the sky the have no distinct cloud units
cumulus.jpg
High clouds
The Cirrus, Cirrostratus and the cirrocumulus make up the high cloud family
They are thin and white often made of ice crystal and can warn of an incoming storm
6506_sm.jpg
Middle Clouds
Clouds that are in the middle have the prefix alto in there name
They are large and dense
middle+clouds.jpg
Low clouds
There are three member s of the low cloud family called the Stratus, Stratocumulus and nimbostratus
There not very thick but they are thicker than cirrus’s
low_level.jpg
Clouds of Vertical development
There are some clouds that do not fit into the categories and are the oddballs of the cloud nation
These clouds are all in relation with unstable air
Once upward movement is triggered from the unstable air these clouds extend upward drastically
Gallery_Image_7708.jpg
Fog by cooling and Evaporation There is not a one difference between fog an cloud Fog is defined as a cloud with its base being near the
ground Fog by cooling happens when the there is a calm clear
night and the earths surface cools rapidly from radiation Fog by evaporation happens when cold air moves over
warm water and is saturated. As the water vapor rises it is immediately condensed and fog is produced
fog_and_truck.jpg
The Bergeron Process
The Bergeron process requires super cooling and super saturation
Super cooled- when water is below 0 degrees celcius Supersaturated- when air is 100% relative humidity When either of these process’s occur a chain reaction of
ice freezing vapor occurs and is transformed into snow
bergeron_s.jpg
The Collision-coalescence process
Collision-coalescence is the mechanism that forms raindrops
Water absorbing particles can remove water vapor from the air at less than 100% humidity, forming large droplets
As the large droplets move through the clouds the gather smaller droplets and eventually fall to earth
Collision.JPG
Rain And Snow
Rain is drops of water that fall from clouds with a diameter of .5 mm
Snow is frozen rain that forms in temps lower than 0 degrees celcius
a1280by1024.jpg
Sleet Glaze and Hail
Sleet is the falling of small translucent ice particles
Glaze is water falling from freezing to subfreezing layered temps that freeze when the water hits the ground
Hail starts out a small ice pellets and grow by hit super cooled water droplets
hail.jpg
THE END!!!!!!!Thank you for you
time, and remember you heard it from the
best!6a00d8341d4dc653ef010536a7be8