Elements of Physical Geography
Lecture 1
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Two instructors, primarily Shambaugh-Miller
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Read the book
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Instructors have a tendency to be informal – grrrr
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Must be because of the limited utility of the field
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Consider and be aware of the scientific method
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facts – simple statement that can be proven
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hypothesis – limited explanation of a phenomeenon
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law – statement about an observed phenomenon or a univfying concept
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theory – in-depth explanation of the observed phenomenon
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Science proves nothing – mathematics, however, does
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Mike needs a copy editor!!
Lecture 2
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Geography in the news
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Hurricane Dorian – another reason not to go to Florida
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Burning rainforest – waiting for apologies
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Pumice raft from undersea volcano
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Life, The Usiverse, And Everything
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How it got here, and where is here?
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"Big Bang Theory"
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Steady-state universe – it has always been here
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Universe expansion may be faster than once thought
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Solar system
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Not understood completely
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4.5—5 billion yo
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Started as a nembula, contracted into protostar, then in sun
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Sun not exact center
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eight planets revolve in elliptical orbits
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for terrestrial, four jovian planets
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Four steps
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protogalactic cloud
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collapses, halo stars form
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angular momentum ensure remaining gas flattens into disk
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star-gas-star cycle supports star formation
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Moon is 1% of Earth's mass
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Moon has no volatiles
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Lecture 3
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Careful of high-pressure systems
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Farmer's Almanac is 64% correct — on par with NOAA/NWS
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The Geographic Grid
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Distortion and geometry — flattening a sphere causes distortion
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Projection — mathematical functionality
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Mercator built on navigation, varies distance of latitude lines, does not preserve size
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Gall-Peters — equal area, distorts chapes
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GPS made many projections less helpful
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Non-rectangular projections used instead
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Winkel-Tripes used by National Geographic
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Recall that the earth is wider at the equator (due to centrifugal force) — means earth is oblate spheroid, wider at the middle by 42 miles
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Consider great-circle routes
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Small-circles are through anywhere except the exact center
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Latitude and Longitude
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Vertical lines denote longitude/meridians
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Horizontal lines are lines of latitude
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Degrees of latitude/longitude at equator are 69 miles
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Degree Minute Second, Degree = 60 minutes, Minute = 60 seconds
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Equator, Tropics (of Cancer and Capricorn), (Ant-)arctic Circle
Lecture 4
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International Geophysical Union changed continents, now Europe and Asia are considered one, Zealandia may become one
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Parallels of latitude: seven major, equator, tropics of Capricorn and Cancer, arctic and antarctic circles, poles
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Cancer is north, Capricorn in the south
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Lincoln is 40.8N, 96.7W
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Axis tilted about 23.5
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Rotation of earth at 1670 kph at equator
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Rotation from west to east (counterclockwise if viewed at the north pole)
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Other systems for lat/long
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What 3 Words
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Plus Codes
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UTM
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Nat'l Grid
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USPS 5 and Plus 3
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PLSS
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Lecture 5
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Earth/sun relationships
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True and magnetic norths converged
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Rotation — spin on an axis (24.25 hr)
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Revolution — movement around a location
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Solstice — sun is directly overhead, sun is at its furthest north/south of the equator
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Tropics — where sun is directly overhead on the two solstices
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Equator — great circle dividing the earth in half at the midpoint between both poles
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Equinox — when sun is directly over equator
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Aphelion — furthest point of sun and Earth
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Perihelion — Closest point of Sun and Earth
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Lincoln solstice is around June 21st
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Aphelion is around July 4th
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Perihelion is around January 4th
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ap-/peri-helion are about 2 weeks after the solstice
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Rotation gives transition from day to night to day
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Tidal effects from the moon and sun
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Coriolis effect causing deflection of winds and currents
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Inclination, 23.5 degrees with regard to the ecliptic, the polarity
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Axis always points to polaris
Lecture 6
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inclination is also known a obliquity
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Sun angle and azimuth
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solar noon – highest solar angle
Lecture 7
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Time is used based on location
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International and Scientific time are slightly different
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DST
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Makes better use of daylight, and saves energy
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Maybe it doesn't work – it's a wash
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No daylight is, in fact, lost
Lecture 8
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Keep in mind dawn and dusk!
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Atmosphere is compressed due to gravity
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Troposphere is lowest, where most weather occurs
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Order, from lowest to highest
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Troposphere
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Stratosphere – location of the ozone layer
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Mesosphere
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Ionosphere/Thermosphere
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Environmental vs atmospheric temperature
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atmospheric is the mean molecular motion of the atmospheric molecules
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Environmental temperature considers overall temperature
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Atmospheric makeup
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Inversions – warm air trapped between cold air
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Clear skies
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calm winds
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long nights
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Types
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Ground
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radiation and advection
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Upper air
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sibsidence, turbulence/convective, trade winds, ozone layer inversion
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frontal
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Impacts
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fog
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pollution
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decreased visibility
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health problems
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economic impacts
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agricultural impact in hilly/mountainous regions
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Lecture 9
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Elements and Control of weather
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Consider angle of incidence and its relationship to latitude
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Distribution of land and water. Water tends to soak up heat more, and hold on to it for longer. Kinda.
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proximity to large bodies of water stabilizes temperature
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Being central to a large land mass implies continental climate
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Atmospheric circulation – very complex
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Wind moves to east in mid latitudes, to west in tropics
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Oceanic circulation has minor influence on weather/climate
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Daily impact of water-land boundaries
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Cool sea breeze during the day
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cool land breze during the evening
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Lecture 10
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heated oceans affect thermohaline
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Altitude – distance from the surface of the Earth, can also be distance from see level
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temp, pressure, moisture all decrease with increasing altitude
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particularly impacts mountanous regions
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Changes vegitation and precipitation patterns
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Topographic barriers – things on the landscape that change the wind patterns
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Mountain/valley winds
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Canyon winds – air goes through because of cooling of canyon walls
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Valley winds – modified direction by forcing through canyon or gorge
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Urban canyon winds – high-speed wind caused by air forced down and through tall buildings
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Weather is confluence of many things
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Coriolis effect – deflection patterns
Lecture 11
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cheesy jokes, test went okay
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Light, why?
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Light from Sun covers wide spectrum.
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Light comes as Electromagnetic radition
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Spectrum, ~7 members
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Visible vs Invisible
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Wavelength, Frequency, Energy
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Low to high
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radio waves
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microwaves
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Infrared
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Visible
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Ultra violet
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X-rays
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Gamma waves
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energy interactions are what matter to weathter
Lecture 12
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Solar radiation, continued
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Radiation heats atmosphere
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Re-emission – long-wave terrestrial radiation
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Emit more than is absorbed, earth cools
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Emit less than is absorbed, earth warms
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What is emitted by surface is absorbed by atmosphere or emitted directly to space
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Can be emitted by atmosphere or clouds
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25% absorbed by clouds, 25% reflected to space, remainder to the planet
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Angle of incidence effects the amount of radiation absorbed per square unit
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Drivers
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Incidennt Angle
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atmospheric Absorption
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Clouds
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Length of day
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Continentality
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large period orbital variation
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Lecture 13
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Trade winds
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Atmospheric Pressure
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Rossby Waves
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Polar Vortex Outbreak
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When the jet stream changes orientation and direction and polar air comes further south than is normal (farther south than 60 north)
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Polar front, 60N, a/k/a polar jet stream
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Become Rossby Waves when very deep
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Atlantic Trade winds
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Doldrums – places where the wind is not
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A/K/A the horse latitudes
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ITCZ, itertropical convergence zone, moves because of seasons and insolation
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Winds are controlled by presure and temperature
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Hawaiian high – persistant, subtropical high pressure
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Azores high between Europe and US (Also called Bermuda High)
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Wind Power Generation
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ITCZ is why monsoon seasons happen
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El Niño – warm phase, warm water, around december, coastal water, wetter weather, warmer in mid and upper plains
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La Niña – cold phase, cold water on wester coast of S. America, normal, drier, colder in mid and upper plains
Lecture 15
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vapor capacity increases exponentially with increase in temp (as does saturation vapor pressure)
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Vapor pressure is the contribution of waer vapor to the total pressure of the atmosphere
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Saturation vapor pressure is the maximum possible vapor pressure at a given temperature
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Saturated air contains more water at warmer temps than does colder temps
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RH affects how we feel temperature
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Dew-point temperature – critical temp at which saturation is reached
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Cooling is most common way air brought to saturation and condensation
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Sensible temperature is a concept of the relative temperature that is sensed by a person's body
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Know
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Absolute Humidity
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Vapor Pressure
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Relative Humidity
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Dew Point
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Sensible Temperature
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Actual Mixing Ratio
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Saturation Mixing Ratio
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Lifting Condensation Level – where the temp and pressure are such that clouds form, altitude at which dew point is reached
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Cloud types
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High
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Cirrus
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Cirrocumulus
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Cirrostratus
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Middle
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Altocumulus
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Altostratus
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Low
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Stratus
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Stratocumulus
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Nimbostratus
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Vertical
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Cumulus
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Cumulonimbus
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Lenticular clouds – get reported as UFOs, hang over mountains etc
Lecture 16
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Discussed Quiz, Exam, Current Course
Lecture 17
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How the Earth Changes
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Energy Influk
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Lifting Mechanisms
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Convective lifting
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As a surface warms, air rises
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Sucks in more air
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Reaches LCL
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then at dew point
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Becomes cloud, may become precip
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Frontal
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Warm air hits cold front
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Looses all moisture
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Convergent
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Warm air sucked in, creates low pressure
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Convective
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Bubble of air that rises
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Precipitation that does not reach the ground is called "verga"/"virga"
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Most precipitation is near the equator
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Condensation nucleus determines pH of condensate
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Alkalinity can happen because of what exists on the land
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Air Masses classified using:
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c – continental
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m – maritime
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P – polar
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A – arctic
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T – tropical
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Lecture 18
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condensation releases heat
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radiation fog is shallow layers near ground
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Fronts
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warm front - gentle, long distance
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cold front - steep, dense
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stationary front
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occluded front - gentle
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fronts come from low pressure centers
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stationary front
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cyclogenesis
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mature cyclone
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occusion begins
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occluded front forms
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fronts dissipate, process restarts
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More distinct the more severe the reaction
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Hurricanes have different names because of history
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Avection is heating over the water
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Eye of storm is indication of strength, more distinct, more strong
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Winds get weaker as you move up
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Storm surge is the biggest issue, causes huge waves
Lecture 19
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Pando is dying, quaking aspin sharing same root system, estimated to be 8000-1000000 years old
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largest living organism
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Even older living things
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Three stages of thunderstorm
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cumulus – development, air gets sucked into storm through lifting mechanism
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mature – upward movement and downward giving heavy rain
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dissipating – dissipating, stops getting air coming in, rains lessen
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Air coming down fastt creates microburst/gust front
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Gust front can roll across the land
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3 times the number of storms over land rather than sea
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Oceans don't release energy fast enough
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Global atmospheric electrical circuit – coure of continuous movemnt of electricity between ionosphere and earth
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solar radiation, thunderstorms, fair weather condition cause continual and substantial electrical current
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Thunderstorms carry negative charges, gradually discharged through air in fair weather
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Electrical imbalance
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elves in thermosphere
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sprites in mesosphere
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blue jets in stratosphere
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lightning, cloud-to-cloud, cloud-to-ground, within cloud, ground-to-cloud in troposphere
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Lightning
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Negative charge in cloud, positive charge on ground
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Cloud can have stratified charges
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5/seconds per mile
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does not need to be close by to strike
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Lake Maracaibo – lightning hotspot
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Intracloud occurs within single thundercloud
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Intercloud, starts and ends between two different thunderclouds
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Cloud to ground, originates in thundercloud and terminates on earth's surface, may occur in reverse
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Positive lightning is more dangerous
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Postive lightning occurs with thundersnows, intense tornadoes, dissipation of a thunderstorm
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Lightning may also occur because of volcanoes, tends to be positive
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Can happen from airplane contrails; rocket engine exhaust; thermonuclear explosions
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Tornadoes
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Mini low-pressure systems – FALSE!!
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Friction with ground causes rolling
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Rolling over warm ground causes avective lifting, which tilts upward
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Physics takes, eventually generating a tornado
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Tornadoes most frequent in May and June
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Nationally, last week of may; Nebraska, mid june
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Fujita scale, measure based on damage, 0 to 5
Lecture 20
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What is the Earth?
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How do mountains get there names? Comes from the culture that names it
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Layers of the earth video
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4000 mi radius
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Different layers
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Each layer has different properties
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As earth cooled, heavy materials sank, lighter materials rose
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Live on the "crust", must be solid, rock and loose material, very thin. 5 mi thick below oceans, 25 mi thick on continents
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Mantle is below, 1800 mi thick, top most is lithosphere, combination of crust and mantle, 60mi thick
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Asthenosphere, 60 mi tthick, semilquid, think silly putty
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Mantle is superheated rock, from 1600F to 7900f in temp
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Outer core, 1400 mi thick liquid layer, mostly iron, 7900F to 110000F, movements create magnetic field
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Inner core, solid layer, 780mi, iron and nickle, solid, may have 13000F temp
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Seismic waves used to determine this
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Differentiation between mantle and crust is called the "mohoriffic discontinuity", or moho
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Ocean vs continental crusts, ocean crust is majority basaltic
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Ocean/continental meeting means lots of energy meeting
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Mantle is largest
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Lava from volcanoes is from lower mantle
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Earth is a dynamo (electrical generator, more or less), generates magnnetic field, protects planet
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Compositional and physical layers
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Physical – divided by solidity/rigidity
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Compositional
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Layers of the earth graphic
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Crust and upper mantle
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Igneous rocks (molten rocks that solidify)
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Intrusive, granite, does not fully break through
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Extrusive, basalt, broke through the crust
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Pluton is an individual lump below the surface that eventualy gets to the surface
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Sedimentary rocks (sediments compact to become solid)
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Weathered rocks, that are later recompressed
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Horizontally layered, called strata
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Limestone tends to come from aquatic life
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Coal is a common organic content
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Shale, sandstone, limestone
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Metamorphic rocks (preasure and heat change the above two)
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Lecture 22
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Pangea and Super Continents
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Overlap of like rock/fossil strata
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Chemical identity of appalachian and caledonian mountains
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Ocean floor mapping
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Late heavy bombardment era – helped to create the plates
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Craton is a stable portion of a continental plate
Lecture 23
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Glaciers, Rivers, Coasts and Climate Change
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Glaciation – when things are covered by glaciers
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Major vs minor glaciations
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Proof of ice ages
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geologic – scouring, scratching, moraines, drumlins
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Chemical – isotopes in folssils
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Paleontological – changes in distribution of fossils
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Peaks and valleys in ice ages
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Glaciations in quatenary
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Gunz/Nebraskan – 2 mya
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Mindel/Kansan – 1.25 mya
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Riss/Illinoisian – 500 kya
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Wurm/Wisconsin – 100 kya
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Causes
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Atmospheric composition
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Large scale orbital cycles (Milankovitch cycles)
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Tectonic plate movement
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Solar output
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Orbital dynamics with regard to the Earth-Moon system
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Impact of meteorites and volcanism
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Pliestocene, 2.59 mybp, ended 11700 ybp
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Rebound – Central CA risen 1000 ft
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Alaska rises at 1.4 in/yr
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Glacial blue due to compression of snow to remove oxygen and other gasses
Lecture 24
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Ablation zone is where things melt (front, tongue)
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Breaking apart
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crevassing
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Ablation speed increases
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Means calving when happens at the front of the glacier
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Glacial Till are the rocks that are brought by the glaciers and left
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Periglacial lakes – those formed by the glaciation as it recedes