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Published byMaurice Evans Modified over 9 years ago
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Climate
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Factors that Affect Climate Climate □Average weather conditions over a long period of time □Defined by Many Factors □Temperature □Precipitation □Latitude □Heat Absorption □Topography
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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
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Example – Mid Latitude
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Example - Tundra
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Latitude □Different Latitudes Receive Different Amounts of Solar Energy □Determines Temperature and Wind Patterns
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Latitude – Solar Energy Solar Energy □Higher Latitudes Receive Smaller Amounts of Solar Energy □Lower Latitudes Receive Larger Amounts of Solar Radiation
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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
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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
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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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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
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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
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Ocean Currents – Ocean Conveyor Belt
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El Nino – Southern Oscillation
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1997-1999
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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
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It Just Started Raining and Raining…
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It Stopped.
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Topography □Recall topography is the surface features of the land □Such features like mountains can control climate □Two Factors □Elevation □Rain Shadows
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Topography - Elevation □As one rises in elevation, the average temperature decreases □Even at the equator the peaks of mountains can be capped with snow
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Topography – Elevation vs. Latitude
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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
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Topography – Rain Shadow
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Topography – Tibetan Plateau
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Types of Climates □Three Distinct Climate Regions □Tropical □Mid - latitude □Polar
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Factors that Affect Biomes
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Climates of the World
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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
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Milankovitch Theory
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Proof is in the Data?
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Potential Impacts Potential Impacts of Climate Change □Global Warming □Sea – Level Changes
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