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Published byLora Thompson Modified over 9 years ago
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Meteorology Basics The study of Weather
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Air Masses Huge masses of air that have uniform qualities of temperature and humidity –cP Continental Polar – dry & cold –mP Maritime Polar – moist & cold –mT Maritime Tropical – moist & warm –cT Continental Tropical - dry & warm
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4 Main Weather Controls Energy from the sun Earth rotates on an axis Earth revolves around the sun Earth is tilted at a 23 ½ degree angle
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Energy Energy from the sun Most important weather control Temperature differences –Tropics are hotter than the poles –This causes convection currents between the poles and the tropics Pressure differences –Warm temps lower pressure –Cold temps higher pressure
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Earth rotates on an axis Coriolis Effect –Is a result of the earth spinning –Anything moving in the northern hemisphere in the air moves to the right (clockwise) –Things in the southern hemisphere deviate to the left (counter-clockwise)
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Earth revolves around the sun This helps give the seasons of the year
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Earth is tilted at a 23 ½ degree angle Causes zones of characteristic winds Causes seasons Temperature differences drive the whole system
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Forecasting Methods Persistence Analog Numerical
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Persistence Forecasting Forecasting for tomorrow the same as what we had today On the average there are 3 days of the same and 1 day of change (the passing front) Correct about 75% of the time
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Analog Forecasting Going back in history to find similar conditions and predicting what the “next” day brought in history
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Numerical Weather Prediction Uses numerical models Involved with computers using energy balance 85-90% accuracy
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Problems with forecasting Surface stations are about 100 mi apart and a lot can happen in 100 mi Atmosphere is three dimensional—what is happening at the surface is often different than what’s happening higher up. Weather balloons etc only measure a tiny portion of the atmosphere at a time. (400mi temp, pressure, wind speed and direction)
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Most important forecasting factor Air pressure measured by a barometer Pressure tendency (rising, falling, steady) gives us some indication about temperature and humidity
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Anticyclone—High Pressure One air mass type Clockwise circulation—due to Coriolis effect Surface divergence Descending air Few, if any clouds No fronts Associated with persistent weather –Hot or cold –No precipitation
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Wave cyclone—Low Pressure Counterclockwise circulation Convergence at the surface Rising air Condensation and precipitation common Different air masses Fronts between air masses
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Comparing Pressure systems
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