where all weather happens, 80% of atmospheric mass, bottom layer
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stratosphere
contains the ozone layer
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mesosphere
coldest layer of atmosphere, where meteors begin to burn up
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thermosphere
temperature increases (inversion), ionization of particles, auroras
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map
models of he environment used to convey information, symbolic representation of space; often have size/shape distortions that are fixed with different projections
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cartography
the art and science of map creation
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space
all the facts and features of a particular location
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latitude
the angular distance, measured in degrees north to south of a point along a parallel from the equator (think latter)
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longitude
the angular distance in degrees east to west of a point along a meridian from the Prime meridian
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scale
ratio of distance on the map to that in real world
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large cell
low resolution/small scale; less detail
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small cell
high resolution/large scale; more detail
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cylindrical map projection
projections of a globe onto a cone; meridians are represented as straight lines radiating from a pole
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conical map projection
projections of a globe onto a cone; meridians are represented as straight lines radiating from a pole
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planar map projection
projections of a globe onto a plane; the plane typically touches the globe at exactly one point; useful for a representation of polar areas
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conformal projection
a map projection in which a small area is rendered in its true shape
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equal area projection
depicts accurate size, but shapes are distorted
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Mercator projection
a map projection of the earth onto a cylinder; areas appear greater the farther they are from the equator
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compromise projection
projections that try to balance out distortions over the entire map
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isoline
a line on a map that connects places that have the same value
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isotherm
a line of constant temperature
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isobar
a line of constant pressure
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GIS
Geographic information system- a system that creates, manages, analyzes, and maps all types of data
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data
includes imagery, features, and base maps linked to spreadsheets and tables
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analysis
lets you evaluate, estimate and predict, interpret and understand
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vector data
includes points, lines, and polygons
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raster data
dats uses an array of cells, or pixels, to represent real-world objects.
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feature
a single entity in GIS that has both geometry, spatial, and attribute data
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which way does the earth rotate?
counterclockwise
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how much is Earth's axis tilted?
23.5 degrees
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what important effects does the rotation of the Earth have on the Earth?
centrifugal force and Coriolis force
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perihelion
earth is closest to the sun (Jan 3)
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Aphelion
earth is furthest from the sun (July 4)
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Kepler's law
the orbit of the Earth is lopsided, one side is a fraction smaller than the other side, so it doesn't make much of a difference in our temperatures.
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why do we have seasons?
Earth's axis tilt
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degree of the equator
0 degrees
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degree of the tropic of cancer
23.5 degrees N
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degree of the tropic of Capricorn
23.5 degrees S
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degree of the arctic circle
66.5 degrees N
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degree of the Antarctic circle
66.5 degrees S
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when is the sun directly overhead the equator?
both the autumnal and spring equinox, every latitude has 12 hors of day and 12 hours of night
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when is the sun directly overhead the tropic of cancer (23.5 N)
summer solstice
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when is sun directly overhead the tropic of capricorn (23.5 S)
winter solstice
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solar declination
the angle between the sun's rays and the plane of the Earth equator
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zenith angles
the angle between the sun and the vertical
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why is it not hot in the arctic circle even thought they have 24 hours of daylight during the summer?
the sun's radiation has more atmospheric mass to get through than in other latitudes
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what is high energy radiation
short wavelengths, higher frequency
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what is low energy radiation
long wavelength, lower frequency
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how much radiation does the sun emit?
400-700 nm (UV spectrum)
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how much radiation does the Earth emit?
7-11 um (infrared spectrum)
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conduction
energy transfer through direct contact of molecules
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convection
the transfer of heat through currents/circulations
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sensible heat
heat you can feel and measure with a thermometer
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latent heat
heat required to change the phase of a substance
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radiation
energy transfer through electromagnetic waves
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insolation
incident solar radiation
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not all of the sun's radiation reaches earth surface due to: (3)
1. absorption 2. transmission 3. redirection (reflected or scattered)
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albedo
the amount of sunlight reflected (scale of 0 to 1)
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net radiation
the total of all radiation (includes incoming and outgoing)
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surplus
excess of energy
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deficit
lack of energy
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how does the greenhouse effect work?
earth radiation heats up the atmosphere because not all of it is released into space some of it it reflected or absorbed by trace gases in the atmosphere.
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weather
short-term conditions of the restless atmospheric systems
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climate
long term conditions of a region
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nitrogen is what percent of the atmosphere
78%
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oxygen is what percent of the atmosphere?
21%
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argon is what percent of the atmosphere
0.9%
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what percent of the atmosphere does trace gases hold?