pressure, fronts, air masses. air pressure the weight of air pressing down on a given area of...
TRANSCRIPT
Pressure, Fronts, air masses
Air Pressure
The weight of air pressing down on a given area of Earth’s surface
Measured with barometer Changes in air pressure
Falling: stormy weather is coming Rising: fair weather is coming Steady: existing weather will continue
WINDWARD SIDE• Warm air cools as it goes over the mountain.• Moisture is released - precipitation
LEEWARD SIDE(other side of the mountain)Cool dry air slides downthe other side of the mountain creating a warm, dry climate.
WIND
LOW ATMOSPHERIC PRESSURE (less)
HIGH ATMOSPHERIC PRESSURE (More)
Warm Moist Air
Warm Air Rises
Warm Air Contracts CoolsMoisture condenses
Moisture is pulled down by gravity
Air rising has released the moisture,And the air becomes warm - less dense. The other side of the mountain will have a great afternoon.
PRESSURE SYSTEMS
HIGH - Clear/fair weather - densely packed molecules warming the air. Warming air decreases relative humidity and water vapor evaporates, before clouds form. Winds turn clockwise and away from center of system
LOW - As warm, less dense air rises, it creates a low pressure system.It forms along fronts where warm air meets cold air, causing a weather change. Stormy weather is associated with low pressure areas.
• Different air masses don’t mix together, when they meet and form a front. • Due to the Coriolis effect, winds begin to swirl counterclockwise in the Northern hemisphere. • Rising air forms a low pressure system, cools, reaches Dew point creating clouds, storms and precipitation.
WARM
COLD
Low pressure
Wind Currents Sun drives convection currents in air Wind is moving air, caused by differences in
air pressure Wind moves from high to low pressure The greater the pressure difference the
greater the wind Local winds=local weather (sea breezes and
land breezes) Global winds= circle Earth in wide belts (jet
stream) Wind vane: determines wind direction; points
to the direction from which the wind is blowing
Anemometer: measures wind speed; Beaufort scale (0-12) relates common observations to wind speed
Local Winds
Sea breeze- convection current blows wind from the cooler sea toward the warmer land during the day
Land Breeze- at night, air moves toward the water as the land cools more rapidly than the water
Ocean Currents
Wind blowing over the ocean’s surface pushing the water, producing a current of seawater
2 types (due to differences in density of seawater) Cold: move from polar regions to
equator Warm: move from tropical equatorial
latitudes to polar regions
Humidity and Dew point Humidity
is the moisture in the air Relative humidity is a comparison of the
amount of water vapor in the air to the greatest amount of water vapor that the air could hold at a given temperature
Psychrometer measure relative humidity Dew point
Temperature when more water vapor is condensing than evaporating-when dew forms
Air Masses
Large body of air that has the same properties as the surface over which it develops.
Maritime Tropical-warm, moist air-forms over ocean
Maritime Polar-cool, moist air-forms over cool ocean waters (north of U.S.)
Continental Tropical- hot, dry air-forms over Mexico, moves north in summer
Continental Polar- cold, dry air-moves into U.S. from Canada in winter
FRONTS - a boundary between 2 different air masses. Clouds, precipitation, and storms occur at frontal boundaries.
Rain occurs at all fronts because warm air is cooled, air becomes saturated and water is precipitated.
COLD COLD FRONTFRONT A cold air mass invades a warm air mass. Cold air
forces the warm air rapidly aloft along the steep front.
Brings violent storms followed by fair cooler weather
COLD AIR
WARM AIRCumulus
Cumulonimbus
The front continues moving in the direction of the cold front.
Cumulus
A warm front develops when a warm air mass meets a cold mass.
Warm air (less dense) advances over the colder air. Brings rain and showers followed by warmer, more
humid weather
WARM WARM FRONTFRONT
COLD AIR
WARM AIR
HOT OVER COLD
NIMBOSTRATUS
ALTOSTRATUS
CIRRUS
The front continues to move along in the same direction.
A STATIONARY FRONT develops when warm or cold front quits moving forward. Often brings many days of almost continuous precipitation.The front does not move - it stays stationary.
COLD orWARM AIR
Weather stays the same.
An OCClUDED FRONT develops when 2 cold air masses merge, forcing the warmer air between to rise. Usually produces heavy rain or other precipitation.
COLD AIR WARM AIR COLD AIR
CUMULONIMBUSSTRATOCUMULUS
Climate vs. Weather
Climate Weather
General weather conditions in broad area over long periods of time, includes seasonal weather changes
Factors in climate Latitude Elevation Topography Distance from water Global winds Ocean currents
The atmospheric conditions in a specific area (within 2 weeks)
Meteorology-study of weather; Meteorologist-studies weather (forecaster)
Factors in weather Convection-uneven
heating and cooling of the Earth’s surface
Air masses-certain temp and amount of moisture
WEATHER FORECASTING
Meteorologists - study and predict the weather.
Station models - show weather conditions at a specific location.
Isotherms - are lines on a weather map connecting points of equaltemperature.
Isobars - are lines on a weather map that connect points of equalatmospheric pressure. Indicates locations of high H and L low pressure systems. Weather fronts move from west to east because of the prevailing westerlies.
Weather Map symbols
STATION MODEL
WIND DIRECTION - TEMPERATURE
CLOUD COVER - BAROMETRIC PRESSURE
SEVERE WEATHER SAFETY
WATCH - means conditions are favorable for severe weather to develop.
WARNING - means that severe weather conditions already exist.
•huge, slowly spinning tropical storm that forms over water•Winds of at least 74 MPH or more (large scale cyclone that causes great destruction to coastal areas)•Winds circulate counter-clockwise•Need warm water temp and moist conditions•Builds energy as it moves across the ocean, sucking up warm, moist tropical air from the surface and dispensing cooler air
Hurricane