chapter 12 meteorology. meteorology = the study of meteors? meteoros = anything high in the air...
TRANSCRIPT
Chapter 12
Meteorology
Meteorology = the study of meteors?
• Meteoros = anything high in the air• Meteorologists study:– Hydrometeors: rain, snow, sleet, hail– Lithometeors: dust, smoke, haze,
particles– Electrometeors: lightning, thunder
• Weather (short term) vs. climate (long term)
Imbalanced heating
• What makes summer warmer than winter?
• Number of hours of daylight and angle of the sun’s rays
Air masses
• Movement of air and water distribute heat around the earth
• Air masses take on the properties of their source regions.– Polar = cold– Tropical = warm– Maritime = humid– Continental = dry– Arctic: very cold/dry
Coriolis Effect
• Moving air curves clockwise in the Northern Hemisphere and counterclockwise in the Southern Hemisphere
• Creates global wind systems:– Polar easterlies– Westerlies– Trade winds
– Horse latitudes– Equatorial low (ITCZ)
Jet Streams
• Narrow bands of fast westerly wind
• Position varies seasonally
• Polar and subtropical• Storms form along jet
stream paths
Weather Fronts
Stationary front
Pressure Systems
• In a low pressure system, air rises, cools and forms clouds
• Air sinks in a high pressure system, usually associated with fair weather
Weather Observation Systems
• Automated surface observing system• Radiosonde (upper atmosphere weather
balloon)• Weather radar (including doppler)• Weather satellites (infrared, visible and water-
vapor imagery)
Weather Data
• Temperature (thermometer)
• Air pressure (barometer)• Wind speed
(anemometer)• Relative humidity
(hygrometer)
Weather Station Models
• A station model is a record of weather data for a specific place at a specific time
• Uniform way of communicating weather data
• Lots of information in a small space
Map with weather stations
Same map with Isotherms
Same map with Isobars
Short and Long Term Forecasts
Short-term• More detailed and accurate• Hourly forecast based on
present weather• One- to three-day forecasts
based on larger systems such as low pressure systems
Long-term• Less reliable because of
great number of variables involved
• Based on large scale circulation patterns and weather cycles