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Physical Geography

Physical Geography. FACTORS THAT AFFECT CLIMATE. http://upload.wikimedia.org/wikipedia/commons/thumb/9/97/The_Earth_seen_from_Apollo_17.jpg/300px-The_Earth_seen_from_Apollo_17.jpg. LACEMOPS. Weather – The daily condition of the atmosphere which includes temperature and precipitation.

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Physical Geography

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  1. Physical Geography

  2. FACTORS THAT AFFECT CLIMATE http://upload.wikimedia.org/wikipedia/commons/thumb/9/97/The_Earth_seen_from_Apollo_17.jpg/300px-The_Earth_seen_from_Apollo_17.jpg LACEMOPS

  3. Weather – The daily condition of the atmosphere which includes temperature and precipitation. Precipitation - Moisture that falls from the sky. Precipitation has 4 forms: rain, snow, sleet, and hail. Climate - Average weather. Measured over an extended period of time (usually 30 years). http://www.mnh.si.edu/archives/garden/images/4seasons.gif

  4. L - LATITUDE - The most important factor! The farther from the Equator - the colder and drier it becomes. Direct rays of the sun are always between the Tropics. Areas not in the tropics receive indirect sun rays. High Mid Low High

  5. A - AIR MASSES In the Northern Hemisphere, cold air from the Polar Regions comes from the north. Hot air from the tropics comes from the south, Mountains to the north of a city could block the cold air from reaching the city. (opposite in the Southern Hemisphere).

  6. C - CONTINENTALITY Water moderates climate. Water takes longer to heat and cool than land. Areas inland from the coast will be hotter in the summer and colder in the winter than areas with the same latitude on the coast. http://images.google.com/imgres?imgurl=http://edc.usgs.gov/imagegallery/imageSrc/United%2520States-NED500.jpg&imgrefurl=http://edc.usgs.gov/imagegallery/imageDetail.php%3Fpage%3D18%26img%3DUnited%2BStates-NED%26id%3D2071%26col%3DStates%2B-%2BNED%2BShaded%2BRelief&h=353&w=500&sz=121&hl=en&start=17&um=1&tbnid=tsJBVC5mQRiZ6M:&tbnh=92&tbnw=130&prev=/images%3Fq%3Dunited%2Bstates%2B%26svnum%3D10%26um%3D1%26hl%3Den%26safe%3Dactive%26rls%3Dcom.microsoft:en-us:IE-SearchBox%26rlz%3D1I7GGLG%26sa%3DG

  7. E - ELEVATION It gets colder as you go up a mountain. The formula for vertical climate is: Temperature decreases 3.5º F for every 1,000 feet increase in elevation (the opposite is also true). You can work out the temperature at the top of a tall mountain. http://images.google.com/imgres?imgurl=http://www.savetibet.org/images/images/MountEverest.jpg&imgrefurl=http://www.savetibet.org/news/newsitem.php%3Fid%3D1050&h=300&w=400&sz=22&hl=en&start=6&um=1&tbnid=ODjU-A29uyNbXM:&tbnh=93&tbnw=124&prev=/images%3Fq%3Dmt%2Beverest%26svnum%3D10%26um%3D1%26hl%3Den%26safe%3Dactive%26rls%3DGGLG,GGLG:2005-42,GGLG:en http://www.commondreams.org/headlines05/images/0314-01.jpg

  8. It is 75º at the base of a 15,000 ft. tall mountain. What is the temperature on top of the mountain? First, count the thousands… (15,000) Second, multiply that number by 3.5… 3.5° (from formula) X 15 (how many thousands of feet the mountain is tall) 52.5° (how much colder at the top than the bottom) Third, Subtract that number from the temperature at the base to get the answer… 75° (temperature at bottom) - 52.5° (how much colder at the top) 22.5 ° (temperature at the top)  Answer

  9. M - MOUNTAIN BARRIERS Orographic effect: Wind containing moisture hits the windward side of a mountain (the side facing the wind). Moisture-full clouds are too heavy to get over the mountain so precipitation occurs, after they’re empty, they are able to rise over the mountain. The side facing away from the wind is called the leewardside. The leeward side of a mountain is arid. The windward side has lush vegetation. The leeward side of a mountain is in the rain shadow and is usually a desert.

  10. O - OCEAN CURRENTS Cold currents bring dry, cool air to the coastal areas. Warm currents bring warm, wet air to coastal areas. http://go.owu.edu/~jbkrygie/krygier_html/geog_111/geog_111_lo/geog_111_lo05_gr/3-16.jpg

  11. P - PRESSURE AND PREVAILING WINDS: Pressure High pressure is heavy, cold air. Low pressure is warm, light air. Heat rises. There are some fairly constant air pressure systems. Notice that these lines are located at 0, 30, 60, 90 (not 0, 23 ½, 66 ½, and 90)

  12. Prevailing Winds The Equator is surrounded by an area of calm called the Doldrums (ITCZ). The Trade Winds (Tropical Easterlies) blow from east to west (generally warm and moist). Westerlies(Prevailing Westerlies). They blow from west to east. The PolarEasterliesblow from 90º in an eastward direction toward the Westerlies. There are serious thunderstorms around the 60º latitude line where the two wind patterns collide http://www.worldstats.org/general_world/maps/prevailing_winds_big.gif Notice that these lines are located at 0, 30, 60, 90 (not 0, 23 ½, 66 ½, and 90)

  13. S - STORMS Where the Polar Easterlies meet the Westerlies there are thunderstorms. When hot air masses and cold air masses collide - there are storms. Cyclonic storms (hurricanes, typhoons, etc.) in the Northern Hemisphere spin counter-clockwise. In the Southern Hemisphere cyclones spin clockwise.

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