Facts: |
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Air Mass Modification |
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| Five Types |
| •Maritime Tropical |
•Continental Tropical |
| •Maritime Polar |
•Continental Polar |
| •Arctic Air Mass |
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•An air mass takes on the properties of the surface it is over. |
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•As an air mass moves to a new location it modifies the surface temperature as much as the surface modifies the air mass. |
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•Air mass modification leads to the heating and cooling of the Earth. |
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Coriolis Effect |
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•Video 1 Anchorage to Miami |
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•Video 2 Argentina to Rio de Janeiro |
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•Video 3 Coriolis Effect and High and Low Pressure Systems |
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Major Wind Systems (web page) |
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•Global Wind Systems |
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trade winds, prevailing westerlies, polar easterlies |
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•Convection Currents |
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| Warming Zone |
Cooling Zone |
| •Warm Air |
•Cool Air |
| •Low Density |
•High Density |
| •Rising Air |
•Sinking Air |
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•Movie on Seasonal Changes (web page): |
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Frontal Systems |
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| A front is the edge of an air mass. |
| •Cold Front |
•Stationary Front |
| •Warm Front |
•Occluded Front |
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Pressure Systems |
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| •High Pressure |
•Low Pressure |
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Gathering Weather Data |
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| Instrumentation Low Level |
| •Thermometer (temperature) |
•Anemometer (wind speed) |
| •Barometer (pressure) |
•Hygrometer (humidity) |
| High Altitude and Technology |
| •Radiosonde (weather balloon) |
•Radar/Doppler Radar |
| Satellites |
| •Photographs |
•Infrared |
| •Radar |
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Using Weather Data |
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| Station Model |
| •A short hand way of putting lots of weather information onto a map. |
| •Stations with similar properties can be joined by a line called an isopleth. |
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-isobars lines of equal pressure |
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-isotherms lines of equal temperature |
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Weather Forecasting |
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•Digital Forecast: using mathematical models to predict weather. |
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•Analog Forecast: using station models and past history to predict weather. |
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•Short term forecast is more accurate then long term. |