Your SlideShare is downloading. ×
Science project
Science project
Science project
Science project
Science project
Science project
Science project
Science project
Science project
Science project
Science project
Science project
Science project
Science project
Science project
Science project
Science project
Upcoming SlideShare
Loading in...5
×

Thanks for flagging this SlideShare!

Oops! An error has occurred.

×
Saving this for later? Get the SlideShare app to save on your phone or tablet. Read anywhere, anytime – even offline.
Text the download link to your phone
Standard text messaging rates apply
0 Comments
0 Likes
Statistics
Notes
  • Be the first to comment

  • Be the first to like this

No Downloads
Views
Total Views
451
On Slideshare
0
From Embeds
0
Number of Embeds
0
Actions
Shares
0
Downloads
3
Comments
0
Likes
0
Embeds 0
No embeds

Report content
Flagged as inappropriate Flag as inappropriate
Flag as inappropriate

Select your reason for flagging this presentation as inappropriate.

Cancel
No notes for slide

Transcript

  • 1. By:Mason Haas
  • 2. Adiabatic temperature changes and expansion and cooling  Air that changes with out heating or cooling.  Dry adiabatic is the rate of cooling or heating in non saturated air  Wet adiabatic rate is the coolinghttp://apollo.lsc.vsc.edu/classes/met130/notes/chapter6/graphics/adiab_warming.gif
  • 3. Orographic lifting  Or graphic lifting of air is happens in elevated terrains like mountain  It acts as a boundary and the air flows up wardhttp://web.mst.edu/~rogersda/umrcourses/ge301/press&siever12.3.png
  • 4. Frontal Wedging  Front is a boundary between were warm and cold air meat  Occurs when cold dence air acts a blanket over the warmer airhttp://www.geography.hunter.cuny.edu/~tbw/wc.notes/4.moisture.atm.stability/frontal.wedging.jpg
  • 5. Localized convection  Occurs when the earths surface heats makes a warm pocket of air warmer then the rest  It lowers the air pockets densityhttp://acd.ucar.edu/~randel/GPS4.gif
  • 6. stability  Air that’s stable usually stays in the same spot  Air that’s unstable usually rises  The most stable air conditions are temperature inversions they are when the temperature of the air goes up with heighthttp://www.revisionworld.co.uk/files/salr_49.gif
  • 7. Condensation  Condensation can only occur if the air is saturated  The types of condensation are dew, fog, and clouds  Condensationhttp://image.shutterstock.com/display_pic_with_logo/235126/235126,1247291688,7/stock-photo-water-droplets-formed-from-condensation-inside-a-blue-bottle-33458629.jpg
  • 8. Cloud types  Clouds are categorized by there height and there form  One type of clouds are cirrus there thin and fluffy  Cumulus are the other type of clouds they are individual  And the last type of clouds are status clouds have layers and cover most of the skyhttp://eo.ucar.edu/webweather/images/cloudchart.gif
  • 9. High Clouds  Three types of high clouds are cirrus, cirrostratus, and cirrocumulus  Cirrocumulus is fluffy  Cirrostratus are thin layers  Cirrus clouds cover the skyhttp://www.bigbranch.net/195.jpg
  • 10. Middle clouds  Middle clouds are any were form 2000 to 6000 meters  They are made up of bigger partials then all the other clouds  They are a grayish coverhttp://www.bigbranch.net/168.jpg
  • 11. Low Clouds  There are three types of low clouds stratus, stratocumulus, and nimbostratus  Stratus clouds are fog like clouds that cover the sky most of the time  Stratocumulus clouds are ling roles  Nimbostratus clouds are rain cloudshttp://image.shutterstock.com/display_pic_with_logo/159841/159841,1285355433,12/stock-photo-landscape-with-low-clouds-above-atlantic-ocean-and-breaking-waves-61627681.jpg
  • 12. Cloud of Vertical development  They are associated with unstable air  They are around in fair wheather  They usually end up making a rain cloudhttp://www.free-online-private-pilot-ground-school.com/images/cloud-types.gif
  • 13. Fog There are two different reasons for fog cooling and evaporation Cooling fog occurs when moist air from the pacific moves over the California current then its pushed on by prevailing winds Fog caused by evaporation happens when cool moves over water if the air gets moist enough fog happens
  • 14. Cold Cloud Precipitation (Bergeronprocess) It’s a theory that relates to the formation of precipitation to super cooled clouds, freezing nuclei, and level difference of liquid water and ice. water in a liquid state under 0 is said to be super cold If super cold water touches an object it will freeze
  • 15. Warm cloud When air is saturated fully it’s the same as ice that’s fully saturated The collision coalescence process is a theory of how raindrops form in warm cloud making cloud droplets collide to for a rain drop
  • 16. Rain and snow The types of precipitation are rain and snow Rain is water falling from clouds when the temperatures is above 4 at the service Snow happens when low temperatures and low moisture and is made up of six sided crystals
  • 17. Sleet, Glaze and Hail Sleet is the fall of clear ice a layer of air has to over line the ground for it to occur Glaze is freezing rain it happens when becomes super cold Hail begins as little ice balls that get bigger when super cold water droplet stick to it as it falls to the surface

×