Air Masses & Fronts - LCPS

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12/14/2010Air Masses &FrontsWeatherAll weather is a result of humidity,condensation and pressure.1

12/14/2010VirginiaGlobalWindPatternsWeather Movement in theContiguous United StatesWe are in the prevailing westerly windbelt, so our weather tends to move fromthe southwest to the northeast.2

12/14/2010Map #1Map #2Map #3Map #4Formation of Waves on SurfaceWaterWind blowing over water produceswaves.3

12/14/2010Formation of Surface OceanCurrentsThe direction of ocean currents isaffected by the prevailing windsbecause the wind blows over the watercausing the currents.Currents tend to spin clockwise in theNorthern Hemisphere andcounterclockwise in the SouthernHemisphere (due to the Coriolis Effect)4

12/14/2010Air MassA large body of air in the lower tropospherethat has similar characteristics throughoutTemperature & humidity depend on originand move with the air massTypes of Air MassesContinental dryContinental:Maritime: wetMaritimePolar: coldTropical: warmcontinental polar (cP): cold & dry (Canada)continental tropical (cT): warm & dry (Mexico)maritime polar (mP): cold & wet (north oceans)maritime tropical (mT): warm & wet (south oceans)5

12/14/2010Types of Air MassesLocal Air Masses6

12/14/2010Weather ExampleContinentalPolarContinentalTropicWeather ExampleCold & dry(no precip)7

12/14/2010FrontsFront- an interface or boundary between 2air masses of different characteristicsFrontsCold Front: boundary between advancing cold air mass & awarmer air mass it is displacing/pushing aside Rising warm air usually produces precipitation if wetAir becomes colder after front passesSteep slopes, rapid changes in weather, thunderstorms, hail, tornadoes8

12/14/2010FrontsWarm Front: boundary between advancing hot air mass & acolder air mass it is displacing/pushing aside 1st clouds days in advance, then RAINAir becomes warmer after front passesGentle slope, long periods of precipitation and layered cloudsFrontsOccluded Front: when cold front ‘catches up’ to awarm front, producing clouds & precipitation as thewarmer air mass between them is forced to rise Forms mid-latitude cyclones (lows)9

12/14/2010Forming an Occluded FrontFrontsStationary front: when a front stops movingforward, producing clouds & precipitation –causes floods if stationary too long10

12/14/2010Fronts and Weather MapsFront Symbols (the symbols point in thedirection the front is moving)Locating a FrontWind direction changesTemperature changes sharplyDew Point changes sharply11

12/14/2010ID That Front!Air Temperature changing as front dfrontch/TAIR10171996.mov)Dew Point Temp changing as front dfrontch/TDEW10171996.mov)Wind Direction changing as front dfrontch/WIND11061996.mov)What type of front is this?Keys to WeatherForecasting(1) Storms move southwest to northeastin US(2) L is stormy, winds arecounterclockwise (low pressure)(3) H is clear, winds are clockwise (highpressure)(4) Precipitation forms near the center of aL and along a front12

12/14/2010Where would precip be?13

Air Masses & Fronts Weather All weather is a result of humidity, condensation and pressure. 12/14/2010 2 Global Wind Patterns Virginia Weather Movement in the Contiguous United States We are in the prevailing westerly wind . Microsoft PowerPoint -

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