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Geography
Study of Earth
1st Step in the Scientific Method
Observation
2nd Step in the Scientific Method
Question
3rd Step in the Scientific Method
Hypothesis
4th Step in the Scientific Method
Experiment
5th Step in the Scientific Method
Conduct Experiment
6th Step in the Scientific
Conclusion
Lithosphere
Outermost rock & mineral matter
Hydrosphere
Vapor, liquid, ice water in air, surface & crust
Bisophere
Distribution of all organisms
Atmosphere
Thin, gaseous veil held to Earth by Gravity
Interaction of Spheres
Interconnected Systems, Equilibrium, Feedback Loops
Interconnected Systems
Change in one system affects another
Equilibrium
Inputs and outputs in balance
Feedback Loops
Outputs “feedback” as inputs reinforcing change
Age of the Universe
13.8 Billion Years Old
Where did the big band theory come from?
Astronomy
Red Shift
Rate of movement speed & distance of other galaxies moving away
Age of our Solar System
4.5 Billion Years
How can we tell the age of our solar system?
Radioactive Decay of elements
Our sun is at the exact center
False - off-center
How many planets are in our solar system?
8
How big is Earth?
24,901 Miles (10 United States)
Deepest Trench
Mariana
Earth’s Shape
Oblate Spheroid
Earth’s Axial Tilt
23.5*
Axis is perpendicular to equator
True
Great Circle
Any plane that bisects a sphere, passing through its center (divided into two equal halves)
Examples of a Great Circle
Hemispheres
Great Circle Route
path between two points along the arc is shortest route compared to straight
Small Circles
Do not pass through Earth’s center
Graticule
Earth’s grid system
Prime Meridian Location
Greenwich England
60 minutes in
one degree
What causes seasons?
Rotation, revolution, axis tilt, polarity
Polarity
north pole stays consistent in the direction it points revolving around the sun
Seasonal changes vary by
latitude
Declination of the sun
latitude receiving vertical ray
Solar Altitude
Sun’s height over the horizon
Tropical latitudes are colder due to high sun angles
False - They are warmer
Polar Latitudes are
cooler
International Date Line
The line marking a time difference of an entire day from on side of the line to the other (180* meridian)
Map is a true depiction of the earth
False - Globe
Map Scale
Relationship between distance on the map & the actual distance on the ground
Types of map scales
Graphic, fractional, verbal
Cylindrical Projection
“Wrap” globe in cylinder
Cons of cylindrical projection
size distortion greatest away from circle of tangency
Mercator Map
Used European imperialist attitudes (1569)
Con of mecator map
distorts size of nations and continents
Planar Projection
project globe onto flate surface at point of tangency
Con of planar projection
typically only shows one hemisphere
Conic Projection
projects globe with base as a standard parallel
Con of conic projection
Distortion of nations & continents further from the point of tangency
Interrupted Projection
minimizes distortion of landmasses by “interrupting” oceanic regions
Goode’s Projection
Interrupted Projection
Isoline
line joining points of equal value
Types of isolines
topographic (elevation contour line), isotherms, isobars, isohyet
Isobars
atmospheric pressurei
Isohyet
precipitation
Digital Elevation Model
shaded-relief digital images showing elevation; shows elevation
Global Navigation Satellite System (GNSS)
GPS
GPS uses trilateration method
measures distances - t*v=s
Remote Sensing
process of detecting & monitoring physical characteristic’s of Earth’s surface & atmosphere from a distance
Electromagnetic Radiation
light measured in photos
Multispectral Remote Sensing
sensing detects and records many wavelengths of the electromagnetic spectrum
GIS
Geographic information systems; computer systems
Radar
Sending a pulse of radio energy off the earth & it comes back
Sonar
Sending a pulse of sound
Lidar
reflected laser light to measure distances & three-dimensional information
Overlay Analysis
two or more layers of data compromised
Blue has the smallest wavelength
true
Size of 50% atmospheric mass
3.8 miles
Density inc/dec with increasing altitude?
decreases
how old is the atmosphere
4 billion years old
How were early gases altered?
volcanic eruptions & comets
Amoebas consumed CO2 and released O2 through photosynthesis
true
How much nitrogen in the atmosphere?
78%
How much oxygen in the atmosphere?
20%
How much argon in the atmosphere?
1%
What are the permanent gases?
Nitrogen, oxygen, argon
Variable Gases
Water vapor, CO2,O3
O3
Ozone found in the stratosphere
Particulates (Aerosols)
larger nongaseous particles
Vertical Layers
Defined based on temperature changes
Troposphere
lowest layer (weather layer)H
How high is the troposphere
5-13 milesS
Stratosphere
Gets warmer, ozone layer
Why does the stratosphere get warmer?
Ozone absorbs the uv energy
Mesophere
Cools down; middle layer
Thermosphere
Particles interact with intense heat of the sun to produce ion, makes it warmer
Exosphere
outermost layer
Air Pressure
Weight of overlying air
where is 90% of the air pressure located?
within 10mi above sea level
Heaviest to lightest
Nitrogen, O2, helium, hydrogen
Ozone hole
severe thinning of ozone at south pole
Primary Pollutants
CO, nitrogen, sulfur (carbon based fuel
Secondary Pollutants
React with UV light (volatile & photochemical smog)
Volatile Organic Compounds
Hydrocarbons & other gases emitted from products or processesT
Types of volatile organic compounds
hydrocarbons, formaldehyde, acetone, chloroform, benzene
Photochemical Smog
forms when nitrogen oxidizes & VOC react to sunlight (brown haze)