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Geography LSU GEOG 2050
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  • Title: Geography
  • Type: Notes
  • School: LSU
  • Course: GEOG 2050
  • Term: Spring

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The Geography science of geography Geography o The science that studies the relationships among natural systems, geographic areas, society, cultural activities, and the interdependence of all these over space Spatial- the nature and character of physical space, its measurements, and the distribution of things within it Geographers use o Spatial analysis Geographers use a method rather than a body of knowledge called spatial analysis Geographers use o Process Set of actions or cechanisms that operate in some special order Physical geography The spatial analysis of all the physical elements and processes that make up the environment: energy, air, water, weather, climate, landforms, soils, animals, plants, microorganisms, and the earth itself Geographers study the relationship between physical geography, and human and cultural geography Earth systems concepts System o Any ordered, interrelated set of things and their attributes, linked by flows of energy and matter, as distinct from the surrounding environment outside the system Systems may be open or closed o Open system Inputs of energy an matter flow into the system, and outputs of energy and matter flow from the system o Closed system A system that is shut off form the surrounding environment so that it is selfcontained o System feedback Feedback loops Outputs function as information that is returned to various points in the system via pathways called feedback loops Negative feedback Information that discourages response in the system Such as giving a plant less light Further production in he system decreases the growth of he system Positive feedback Feedback information encourages increased response in the system Further production in the system stimulates growth in the system System equilibrium When the rates of inputs and outputs in the system are equal and the amount of energy and matter in storage within the system are constant o Called a steady-state equilibrium Dynamic equilibrium Changing trend over time, these changing trends of either decreasing or increasing system operations may appear gradual Threshold Point which it can no longer maintain its character, so it lurches to a new operational level Abrupt changes places the system in a metastable equilibrium Earths four spheres Atmosphere, hydrosphere, lithosphere, biosphere Abiotic systems (nonliving) o Atmosphere Thin, gaseous veil surrounding earth, held to the planet by the force of gravity o Hydrosphere Earths waters, on the surface, and in the crust, in all three states (gas, frozen, liquid) Cryosphere The portion of he hydrosphere that is frozen o Lithosphere Earths crust and a portion of the upper mantle directly below the crust Broadly refers the entire solid planet Biotic system (living) o Biosphere Interconnected web that links all organisms with their physical environment Sometimes called the ecosphere, is the area in which physical and chemical factors form the context of life It exist in the overlap among the abiotic spheres Earths dimensions Polar circumference o 40,008 km (24,860 miles) Equatorial circumference o 40,075 km (24,902 miles) the area where the earth extends outside the sphere is called the Geoidal bulge o Earths equatorial girth is expanding slightly with the seasons as the crust compresses a little each hemispheres winter Location and time on earth Latitude o The angular distance north or south of the equator o Parallel A line connecting all points along the same latitudinal angle o Latitude is the name of the angle and parallel names the line Example: 49 degrees north latitude, and 49th o parallel Latitude can be found by sighting Polaris and measuring the angle towards the horizon o Lower latitudes are near the equator and higher latitudes are those nearer the poles o Know the names of the geographic zones Longitude o An angular distance east or west of a point on earths surface o Meridian A ling connecting all points along the same longitude o Longitude is the name of the angle, and meridian is the name of the line, such as the prime meridian Great circles o Any circle of earths circumference whose center coincides with the center of earth o Every meridian is one-half of a great circle that passes through the poles Only one parallel is a great circle, and it is the equatorial parallel Small circles o All other parallels diminish in length toward the poles and, along with any other non-great circles Maps, scales, and projections Map o A generalized view of an area o Cartography- part of geography that involves mapmaking Scale o Relates a unit on a map to a similar unit on the ground Example: 1:1 scale means one centimeter on the map represents a centimeter on the ground The higher the second number the smaller the scale When expressed as a fraction it is called a representive fraction Graphic scale Or bar scale is a bargaph with units to allow measurement of distance on the map, it advantage is it enlarges and reduces with the map Projections o A globe is the only true representation of distance direction, area, shape, and proximity o The reduction of the spherical earth to a flat surface is called a map projection No flat projections can ever have all the features of a globe o There is a trade off between equal area, and true shape when using a projection o Mercator projection A cylindrical projection Distorts size, but keeps the true shape o Rhumb lines Advantage of the mercator projection is that lines of constant direction are straight and thus facilitate plotting directions between two points Remote-sensing Information about a distant subject with having physical contact Such as aerial photographs, called photogrammetry Active remote sensing o Direct abeam of energy at a surface and analyze the energy reflected back o Such as radar Passive remote sensing o Record energy radiating from the surface, particularly visible light and infrared o Such as studying a volcano from a satellite Geographic information systems (GIS) A computer based, data processing tool for gathering, manipulating, and analyzing geographic information Capable of analyzing patterns and relationships within a single data plane, such as a floodplain, soil layer, parcels, zoning ,wetlands, and landcover Week 2 notes Composition and structure of the earths atmosphere Meteorology o Study of weather Why do clouds form, ect o Weather What will happen within the next 2 weeks Climatology o Typical conditions for a particular place for some time period of interest The thickness of earths atmosphere 5.14 x 10^15 kg is the weight of the earths atmosphere the higher up you go the less atmosphere material present, therefore the atmosphere is less dense most of the air is contained in the thin layer near the surface called the troposphere which goes up to 50 km above earth (90 percent) nasa defines everything higher than 62 miles is considered out of the atmosphere Composition of the atmosphere gases solid or liquid particles ice crystals and water stable and variable components o example: nitrogen is a stable component because it remains 72 percent of the earths atmosphere o ozone, methane, carbon dioxide, and water vapor are not stable, and vary between regions

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