Air Mass - a body of air that covers a relatively wide area and exhibits horizontally uniform properties
Atmosphere - the air surrounding and which is bound to the Earth
Conduction - flow of heat in response to a temperature gradient within an object or between objects that are in physical contact
Convection - the transfer of heat within the air by its movement
Used specifically to describe the vertical transport of heat and moisture, especially by updrafts and downdrafts in an unstable atmosphere
Clouds - a visible aggregate of minute water droplets or ice particles in the atmosphere above the Earth's surface
Mesosphere - the atmospheric shell between about 20 km and about 70 to 80 km, extending from the top of the stratosphere (the stratopause) to the upper temperature minimum that defines the mesopause (the base of the thermosphere)
Ozone - a form of oxygen in which the molecule is made of three atoms instead of the usual two
Usually found in the stratosphere
Responsible for filtering out much of the sun's ultraviolet radiation
Primary component of smog
Stratosphere - the region of the atmosphere extending from the top of the troposphere to the base of the mesosphere
Important area for monitoring stratospheric ozone
Thermosphere - the atmospheric shell extending from the top of the mesosphere to outer space
Temperature increases steadily with height
Tropical - areas of the Earth within 20 degrees North and South of the equator
Troposphere - the layer of the atmosphere from the earth's surface up to the tropopause
Decreasing temperature with height, vertical wind motion, appreciable water vapor content, sensible weather
Water Vapor - a dispersion, in the air, of molecules of water, especially as produced by evaporation at ambient temperatures rather than by boiling
Atmosphere:
Nitrogen (78.1%) - dilutes the oxygen and is used by living things to make proteins
Oxygen (21%) - used by nearly all living things for respiration
Argon (0.9%) - used in light bulbs and double pane windows
Carbon Dioxide (0.035%) - used by plants to make oxygen, serves as a blanket for the earth to hold in heat
As you travel up through the atmosphere, moving toward space, the temperature changes and the air pressure decreases and become thinner.
Layers of the atmosphere:
A) Thermosphere
B) Mesosphere
C) Stratosphere
D) Troposphere
E) Mesopause
F) Stratopause
G) Tropopause
Exosphere
outermost layer
375-6200 miles above the earth
low air density, molecules escape into space
Thermosphere
53-375 miles above the earth
air is still thin but becomes denser moving closer to earth
temperature increases as height increases due to UV light and radiation
Mesosphere
31-53 miles above the earth
temperature decreases (moving toward space)
gasses are dense enought to slow meteors
Stratosphere
Troposphere-31 miles above the earth
temperature increases (moving away from earth)
Troposphere
4-12 miles from earth
where weather occurs
temperature decreases
As elevation increases, air pressure decreases
Air pressure is usually measured using a barometer and recorded in “inches of Mercury” or “millibars”
Movement of Heat:
A) Radiation
B) Convection
C) Conduction
Frontal Boundary - a boundary or transition zone between two air masses of different density, and thus (usually) of different temperature
A moving front is named according to the advancing air mass
Jet Stream - relatively strong winds concentrated in a narrow stream in the atmosphere, normally referring to horizontal, high altitude winds
Position and orientation of jet stream vary day to day
General weather patterns are related closely to the position, strength , and orientation of the jet stream(s)
Air Mass
First Part of Name - Location:
Maritime - air mass over ocean
Continental -air mass over land
Second Part of Name - Temperature
Arctic - closest to the poles, considered frigid
Polar - cold areas
Tropical - warms areas, close to the equator
continental-Tropical (cT) - form over deserts, hot and dry
continental-Polar (cP) - form over cold, dry land
continental-Arctic (cA) - form over frozen land, coldest and driest
maritime-Tropical (mT) - form over water, warm and humid
maritime-Polar (mP) - forms over cold water, cold but humid
Front - boundary between two air masses with different temperatures and moisture contents
Often cause active weather events
Stationary Front:
when a front stops moving
noticeable differences in temperature and winds on either side of the front
begins moving again, it resumes its cold/warm front status
Cyclones moving along a stationary front often produce a lot of precipitation
Occluded Front:
A cyclone forms when a cold front overtakes a warm front, the warm air is occluded from the center of the cyclone
Cold Front:
area where a cold (and dry) air mass is replacing a warm air mass
generally move from NW to SE
Warm Front:
area where a warm (and humid) air mass is replacing a cold air mass
generally move from SE to NW
Dry Line:
Separation of a dry air mass from a moist air mass
Big difference in humidity
Dry air behind the dry line lifts the moist air ahead of it which creates thunderstorms
Types of Clouds:
Cirrus - wispy, composed of ice crystals. Found at higher altitudes and can be seen ahead of a low pressure system (ex. Hurricane)
Cumulus - fluffy, dense with flat bottoms which designate the altitude where moisture begins to condense
Stratus - flat and broad
Nimbus - rain clouds
Types of Precipitation:
Snow - water vapor that freezes and falls to the ground
Sleet - snow that melts and then refreezes when it hits the ground
Freezing Rain - snow that melts and then refreezes when it hits the ground
Hail - begins as frozen water and falls through the atmosphere, an updraft catches the ice and pushes it back up where it collects more water that freezes
Cyclonic Storm - a thunderstorm that undergoes cycles of intensification and weakening (pulses) while maintaining its individuality
Capable of producing multiple tornadoes or bursts of severe weather
Relative Humidity - a dimensionless ratio, expressed in percent, of the amount of atmospheric moisture present relative to the amount that would be present if the air was saturated
Function of moisture content and temperature
Does not indicate actual amount of atmospheric moisture present (dew point)
Increase air pressure by adding more molecules and warming the temperature
More movement, lower pressure
When air pressure decreases, it indicates:
hot weather - thunder
fair weather - high winds
cold weather - thaw
When air pressure increases, it indicates:
winter - frost
frosty - snow
wet weather - fair weather
High-Pressure
high pressure in the middle
blows clockwise
calm day with no rain
Low-Pressure
low pressure in the middle
blows counterclockwise
cloud, hurricanes, typhoons
With the unstable air moving, positive and negative charges build and quick discharge of electricity is released - lightning.
The temperature rises so quickly that it causes the air to expand creating a sound wave - thunder.