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78 Cards in this Set

  • Front
  • Back
latitude
runs N or south of the equator - parallel
longitude
lines join N and S poles together
O degrees longitude
Prime Meridian - greenwich England
180 degrees longitude
International Date Line - divides earth into E and W
23.5 degrees N Lat
Tropic of Cancer
23.5 degrees S Lat
Tropic of Capricorn
The path earth travels around the sun
Revolution
The earth's rotation on its axis
Rotation
Plane of the Ecliptic
The earth travels in a constant plane around the sun
Inclination of the earths axis
The imaginary earth axis that is parallel with the equator it is 66.5 degrees to the actual earths axis
Vertical Rays of the sun
--Sun's rays perpendicular more concentrated light
-- sun's rays at greater angle light is spread out
Vertical Rays 23.5 degrees N
Jun 21
Summer Solstice
Vertical Rays 0 degrees
Sep 21
Autumn Equinox
Vertical Rays 23.5 degrees S
Winter Solstice
Vertical Rays 0 degrees
March 21
Vernal Equinox
Statement Scale
EX: 1 inch to 5 miles
Bar Scale
Shows picture of bar 10 miles / 30 miles
Representative Fraction
Map distance/(over)land distance
The labels must be the same
EX: inches/inches
Insolation
Incoming solar radiation that hits the earth's surface
Reflection
ability of an object to to repel waves
Absorption
the ability of an abject to assimilate enoergy from waves that strike it
Scattering
When wavelengths are deflected.. change in direction
Transmission
The ability of a medium to let rays pass through
--Soil BAD
--Water GOOD
Convection
Vertical Movement of parcels of air
-- warm air RISES
-- cold air SINKS
Conduction
The movement of energy from one molecule to another
Advection
Heat being transfered laterally in the atmosphere
--mostly by winds
Radiation
Process by which energy is emitted
Energy Budget
Earth absorbs 48% of sun's rays
persistant shift of :
--warmth poleward
--coldness equatorward
Mechanisms of heat transfer
Poleward Oceanic Circulation
Western side of ocean basins
warm water is carried toward higher latitudes
Equatorward Oceanic Circulation
Moving currents of the Eastern side of oceans - carry cool water toward lower latitudes
Vertical temperature patterns
Temps decrease as we move up in atmosphere
normal lapse rate of vertical temps
average loss of 3.6 degrees per 1000 ft
Lines that connect certain somthings
Isolines
Lines connects certain temperatures
Isoterms
The weight of the overlying air
Atmospheric Pressure
Horizantal movement of air - also called advection
WIND
Nature's Attempt to even out the unever distribution of air pressure over the earth
WINDS
Causes in Direction of Wind Movement
Pressure Gradient
Coriolis Effect
Friction due to earth's surface
Pressure Gradient
Air movement HIGH 2 LOW
Coriolis Effect
Delfection of air:
--2 the RIGHT in NH
--2 the LEFT in SH
Geostrophic Winds
Winds that travel parallel to isobars
High Pressure Systems
Air is sinking and Diverging

GOOD WEATHER
Anticyclones
Low Pressure Systems
Air is Rising and Converging

CLOUDS AND PERCIPITATION
Cyclones
Side of mountain good for percipiation air is rising
Windward side
Side of mountain that is dry air is sinking
Leeward side
Role of Moisture in the Atmosphere
--Evaporation
--Condensation
--Precipitation
Hydrologic Cycle
Stored Heat
Latent Heat
Water Vapor transforming back into a liquid
--Air must be satuarated for this to occur
Condensation
Rate of temp as it moves into the atmosphere 3.6 degrees/ 1000 ft
Normal Lapse Rate
Air cools as it rises
Constant rate of 5.5 degrees/1000 ft
Dry Adiabatic Lapse Rate
After condensation occurs heat is released this slows rate of cooling to 2 degrees/1000 ft
Saturated Adiabatic Lapse Rate
Radiation Fog
Often occurs in mid lats on COLD and CLEAR nights
Advection Fog
Warm moist air moves over snow-covered ground or cool ocean current
Evaporation Fog
Addition of water vapor to cold air that is already saturated
Requirements of an Air Mass
--1000 miles in diameter
--several miles deep
--adjacent to earths surface
Warm Front
--edge of an advancing warm air mass
--Precip falls in front of
Cold Front
--leading edge of cool air mass that is displacing warm air
--move fast
--more intense weather and precip.
Stationary Front
Niether air mass is replacing the other
Large migratory low-pressure systems that occur in the mid-lats
Extratropical Cyclone
Major Occurance in the Westerlies
-Extensive migratory high-pressure cell
Extratropical Anticyclone
Major tropical Disturbance- low-pressure
Responsible for Hurricanes/Typhoon/Cyclone
Tropical Cyclone
Thunderstorms
--Can occur with any lifting mechanism
--Always associated with with vertical air and instability
3 Stages of Thunderstorm Development
1. Cumulus
2. Mature
3. Dissipation
Smallest of all Atmospheric Disturbances
Most Distructive
Tornado
This is based on observed data
Empiric Classification
This is based on factors that cause climate
Genetic Classification
Zone of Aeration
Contains Air
Soil Water
Zone of Saturation
All spaces filled with water
Ground Water-- Water Table
Zone of Confined Water
Water that is separated by an impermeable rock layer
Obliquity
The angle between the plane of the Earth's orbit and the plane of the Earth's equator; the "tilt" of the Earth.
Precession
The tendency of the Earth's axis to wobble in space over a period of 23,000 years.
Orbital Eccentricity
The degree to which an elliptical orbit is elongated.
Hydrosphere
Portion of a planet that is water, including liquid water, ice, and water vapor on the surface, underground, or in the atmosphere.
Aquiclude
A geologic formation which may contain water but does not transmit it.
Lithosphere
the solid part of the Earth below the surface, including any ground water contained within it.
Divergent Plate Boundries
Oceanic ridges
New sea floor material is being added
--Plates are moving away from each other
--Earthquakes and volcanic activity
Convergent Plate Boundries
--Plates meet
--On edges of ocean basins, crustal material subducted and melted
--Considerable earthquakes ad volcanic activity