W. Parker Jackson Climatology. Goals for this Presentation Teach myself how to use Power Point To...

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W. Parker Jackson Climatology

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Pretty picture of the Water Cycle®

Transcript of W. Parker Jackson Climatology. Goals for this Presentation Teach myself how to use Power Point To...

Page 1: W. Parker Jackson Climatology. Goals for this Presentation Teach myself how to use Power Point To show you the amazing world of the hydraulic cycle To.

W. Parker JacksonClimatology

Page 2: W. Parker Jackson Climatology. Goals for this Presentation Teach myself how to use Power Point To show you the amazing world of the hydraulic cycle To.

Goals for this PresentationTeach myself how to use Power PointTo show you the amazing world of the

hydraulic cycleTo re-educate you on things you learned in

intro to Geography and have since forgottenI would love to make this learning experience

fun and entertainingContinue the trend of making fun of Al Gore.

Page 3: W. Parker Jackson Climatology. Goals for this Presentation Teach myself how to use Power Point To show you the amazing world of the hydraulic cycle To.

Pretty picture of the Water Cycle®

Page 4: W. Parker Jackson Climatology. Goals for this Presentation Teach myself how to use Power Point To show you the amazing world of the hydraulic cycle To.

The 3 Major Components of the Water Cycle

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Which comes first?

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Evaporation This the first step in the water cycle. Occurs

when the water in oceans, lakes, rivers, streams, puddles, swimming pools, or any other concentration of water is warmed up by the Sun. The heat adds energy to matter. This in turn causes the molecules to move faster, bouncing off of each other, they move further and further apart till they become gaseous. The water then becomes, vapour.

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Most ill picture of Evaporation I could find on the interweb

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2nd Graders’ Picture of Evaporation

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Another over simplified example of Evaporation

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Condensation

Once the sun heats the water molecules to the point where they become a vapour in the air, this warm air then rises high into the atmosphere where temperatures are a lot colder. The air cools down and the vapour turns back into water. This is where clouds are formed. Yay clouds!

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Good Condensation

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Bad Condensation

You best be usin a coaster under that glass!

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Good Idea, Lance. Thank you.

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Fog

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Great South American Exports

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The Humboldt Current

Discovered by Alexander Von Humboldt(Prussian)

It creates year round upwelling in Peru. Not so much in Chile

Approximately 20% of the worlds fish catch comes from this Large Marine Environment

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Advection FogChilean Coast Californian Coast

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California Coast FogLos Angeles San Francisco

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PrecipitationWhen a large enough amount of water droplets form 'inside' a cloud, they become heavy enough to fall to Earth. This is usually observed as rain, but Precipitation can also occur as snow, hail, sleet, etc., depending on temperatures and humidity.

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3 most common forms of Precipitation

SnowRainHail

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Snow

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Real Snow

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Snow in action

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Science and recreation on the snow

Testing the snow pack Snowboarding and skiing

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Justin Bieber

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Hail

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Hail

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Hail flow chart

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Front Symbols

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What happens when warm air and cold air meet?

When a front of cold air, which is low pressured, moves over a front of warm air, which is high pressured. The friction of the cold air sinking and hot air rising creates high wind speeds and the winds follow the path of the cold air spiraling down.

In short a tornado may occur.

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Tornado

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Cool picture of a tornado

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Tornado map

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Where does all this precipitation go?

Drainage and runoff

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Drainage Patterns

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Drainage PatternsDentritic; basic drainage. Tributaries coming

together to form a larger riverRectangular; this form of drainage is most

common in areas with lots of fault linesAngular or radial; This drainage is at the peak of

the mountain or hillTrellis; multiple small sources flow into a larger

body at almost an acute angleContorted; this type of drainage appears in areas

where there has been much change in the geography of the land

Parallel; many tributaries come together on a more steep then usual downhill slope

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Most Common Patterns Dentritic Parallel

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More DrainageTrellis Angular or radial

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More DrainageContorted Rectangular

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Shoulda stayed home, Al.

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The endAuf wiedersehden Chus!