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Climate. Factors that Affect Climate Climate □Average weather conditions over a long period of time □Defined by Many Factors □Temperature □Precipitation.

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Presentation on theme: "Climate. Factors that Affect Climate Climate □Average weather conditions over a long period of time □Defined by Many Factors □Temperature □Precipitation."— Presentation transcript:

1 Climate

2 Factors that Affect Climate Climate □Average weather conditions over a long period of time □Defined by Many Factors □Temperature □Precipitation □Latitude □Heat Absorption □Topography

3 Temperature and Precipitation □Two Ways to Measure Temperature □Average Monthly Temperature □Yearly Temperature Range □Two Ways to Measure Temperature □Average Monthly Precipitation □Yearly Precipitation Range

4 Example – Mid Latitude

5 Example - Tundra

6 Latitude □Different Latitudes Receive Different Amounts of Solar Energy □Determines Temperature and Wind Patterns

7 Latitude – Solar Energy Solar Energy □Higher Latitudes Receive Smaller Amounts of Solar Energy □Lower Latitudes Receive Larger Amounts of Solar Radiation

8 Latitude – Global Wind Patterns Global Wind Patterns □Results from the uneven heating of the Earth □Warm Air Creates Low Pressure (Equator) □Cold Air Creates High Pressure (Poles) □Results in Wind

9 Heat Absorption and Release □Different areas differ in how they absorb and release heat □Water Absorbs and Releases Heat at a Slow Rate □Hence the reason for our late spring □Land Absorbs and Releases Heat at a Faster Rate □Influences the amount of heat available to heat the land

10 Heat Absorption and Release Controlled by the Following □Specific Heat of Water and Land □Evaporation Rates □Ocean Currents □El Nino – Southern Oscillation □Seasonal Winds

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12 Heat Absorption - Specific Heat and Evaporation □Water has a high Specific Heat □The amount of energy required to raise the temperature of water one degree Celsius □Evaporation □Temperature Changes of Land and Sea vary because of Evaporation □Evaporation affects Water more than it does Land

13 Heat Absorption - Ocean Currents □If wind from the water is blown towards shore it will greatly influence the weather on the land □EX. Northwest Europe and Gulf Stream □El Nino – Southern Oscillation □El Nino – Warm Water Phase □La Nina – Cool Water Phase □Has Global Impact on Weather □3 – 10 Year Cycle

14 Ocean Currents – Ocean Conveyor Belt

15 El Nino – Southern Oscillation

16 1997-1999

17 Heat Absorption - Monsoons □Caused by the Differentiated Heating of Land and Water □Summer □Land warms faster than water □Warm air rises over land and is replaced by cool ocean air □Rain □Winter □Land cools faster than water □Cool air over land is flows away from land □Drought

18 It Just Started Raining and Raining…

19 It Stopped.

20 Topography □Recall topography is the surface features of the land □Such features like mountains can control climate □Two Factors □Elevation □Rain Shadows

21 Topography - Elevation □As one rises in elevation, the average temperature decreases □Even at the equator the peaks of mountains can be capped with snow

22 Topography – Elevation vs. Latitude

23 Topography – Mountains □Mountains cause air masses to rise □As air masses rise the cool and loose their moisture □Results in lush vegetation on windward side of the mountain, and desert on leeward side of the mountain □Examples □Alps □Himalayans □Sierra Nevada

24 Topography – Rain Shadow

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26 Topography – Tibetan Plateau

27 Types of Climates □Three Distinct Climate Regions □Tropical □Mid - latitude □Polar

28 Factors that Affect Biomes

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32 Climates of the World

33 Global Climate Change Potential Causes of Global Change □Plate Tectonics □Disrupt Ocean Currents □Disrupt Wind Patterns □Orbital Changes □Milankovitch Theory □3 Motions on a 20,000 – 100,000 Year Cycles □Human Activity □Carbon Dioxide □Volcanic Activity

34 Milankovitch Theory

35 Proof is in the Data?

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37 Potential Impacts Potential Impacts of Climate Change □Global Warming □Sea – Level Changes


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