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Weather. Click HERE for Discovery Channel Guide to Extreme Weather (50 min). Weather -It’s what’s happening outside NOW!. Weather. All weather is a result of humidity, condensation and pressure. Water Cycle. Humidity—Water Vapor in the Air.
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Click HERE forDiscovery ChannelGuide to Extreme Weather (50 min)
Weather All weather is a result of humidity, condensation and pressure.
Humidity—Water Vapor in the Air • Specific humidity: actual amount of water vapor in the air at a given time & place (grams of vapor per kilogram of air) • Warmer air can hold more water vapor
Humidity Relative humidity: how close the air is to reaching its maximum capacity of water vapor • expressed as a percentage • 100% means it has reached maximum capacity
Humidity Measured with a psychrometer A psychrometer has two thermometers to determine humidity. The dry bulb thermometer measures the room temperature, and wet bulb thermometer is wrapped in a wet cloth. Air is passed through the psychrometer to evaporate moisture on the wet bulb. The readings on the dry bulb thermometer and the wet bulb thermometer are then compared to determine the actual humidity.
Condensation When water changes from a gas to a liquid • Dew point: the temperature at which the air becomes saturated with water vapor & condensation occurs • If air cools below the dew point, water starts condensing into a liquid, forming dew or cloud droplets
Condensation • Fog & clouds form only when there are condensation nuclei (like dust particles) for the water to condense on • Air must cool below its dew point
Smog over LA from car exhaust
Cloud Formation • When warm, wet air from the surface rises, it begins to cool. Eventually, the temperature drops to its dew point, and the water vapor can condense onto the condensation nuclei • Condensation level: the atmospheric level at which condensation occurs
Warm air rises taking the water vapor along with it. Once it cools, it condenses forming a cloud.
Cloud Types Classified by altitudeand shape
Cloud Types Stratus: clouds that form inlayers Cirrus: high,featheryice clouds Cumulus: fluffyclouds with flat bases Nimbus: darkrainclouds
Precipitation Any form of water that falls from a cloud to Earth’s surface
Types of Precipitation • Rain • Snow • Sleet: raindrops that refroze on their way to the surface • Freezing Rain: raindrops that only freeze when they hit the surface • Hail: when frozen raindrops are bounced up & down in the cloud until they fall in a huge ball of ice
Types of Precipitation depend on the temperature of the atmosphere, both at the surface & on the way down snow sleet freezing rain
Measuring Precipitation • Rain gauge: measures liquid precipitation • Measuring stick: measures frozen precipitation
Where is Precipitation? Rain Shadow effect: near a mountain range, the windward side gets lots of rain and the leeward side gets little/no rain – the rain shadow
Extreme Weather1 minute video • http://science.discovery.com/videos/against-the-elements-mashups-devastating-winds.html
Air Mass • A large body of air in the lower troposphere that has similar characteristics throughout • Temperature & humidity depend on origin and move with the air mass
Types of Air Masses Continental: dryPolar: cold Maritime: wetTropical: warm • Continental polar (cP): cold & dry • Maritime polar (mP): cold & wet • Continental tropical (cT): warm & dry • Maritime tropical (mT): warm & wet
Fronts • Cold Front: boundary between advancing cold air mass & a warmer air mass it is displacing • Rising warm air usually produces precipitation if wet • Air becomes colder after front passes
Fronts • Warm Front: boundary between advancing hot air mass & a colder air mass it is displacing • 1st clouds days in advance, then RAIN • Air becomes warmer after front passes
Fronts • Occluded Front: when cold front ‘catches up’ to a warm front, producing clouds & precipitation
Fronts Stationary front: when a front stops moving forward, producing clouds & precipitation – causes floods if stationary too long
Locating a Front • Wind direction changes • Temperature changes sharply • Dew Point changes sharply
Weather Forecasting • Satellites • Radiosondes • Surface observations
Forecasting • Computer models take current data & plug it into equations to predict weather • Meteorologists take computer models & tweak them to fit their experience with local conditions
Forecasting Trend Method: using past movement of a front & precipitation to predict future movement