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Physical Geography 1

QuestionAnswer
Atmosphere gases essential to live -composed of nitrogen and oxygen
Lithosphere (earths crust) solid, rocks and minerals
Whats Geography? -an ancient inter-disciplinary study. -study spatial patterns on earths surface, physical aspect of earth (including temp)
What do most Geographers refer to themselves as? physical or human
Physical Geographer climatology, hazards, geomorphology, soils, etc
Human Geographer regional development, economy, political geography, etc.
Biosphere plants and animals (where we live)
Hydrosphere water
earth-sun relationship energy that flows from the earth and the sun
which sub-disciplines of geography use spatial analysis? climatology, geomorphology, soils, meteorology, geology, biogeography, ecology, hydrology (ALL OF THEM)
Big misconception of geography? not just places and locations
great circles N&S direction, converge at the poles -longitude/meridian lines
small circles N&S of the equator have smaller diameters, always parallel -latitude/parallel lines tropic of cancer,tropic of capricorn
latitude zones arctic, sub-tropic, mid-latitude (35N/S-55N/S) sub-latitude (25N/S-30N/S)
Maps basic tool of geographer
Cartography (study of map making) focus on ways to display spatial information so it can be used and understood efficiently
Map distortion distort shape, distance, area, direction, etc.
Globe most accurate (least distorted)
Conformal distorts area, maintain shape; right angles at each line of latitude -maintains correct shape of earths features, but distorts relative size
Equivalent accuratly portrays size features throughout map
Map Scale relates to size and distance between features on a map to actual features in the real world
Large Scale Map shows smaller area in greater detail
Small Scale Map shows larger area in little detail
Isoline Maps lines connection point of equal value on a map
Isobars point of equal atmospheric pressure
Isotherms point of equal air temprature
Isohyets point of equal parcipitation amounts
Isopachs point of equal sedimentary thickness
Contours point of equal elevation -the closer the spacing of contour lines, the steeper the slope
Sun-synchronus Orbit keeps pace with the sun (West to East)
Geostational Orbit permanatley remains in one place above earth, directly above the equator
Geographic Information System (GIS) used for storing, analyzing, and visualizing spatial data used for: road work, delivery routes, mail, school busing, traffic, etc.
Sun Energy earth receives 50% of one billionth of the suns energy
Milky Way Galaxy the spiral collection of stars that include our solar system
Temperture of the sun 6,000 degrees celcius
Sub-solar Point suns rays are perpindicular to earths surface (moves with seasons)
Perihelion winter, point of orbit closest to the sun
Alpihelion summer, point of orbit farthest from the sun
Circle of Illumination boundary between day and night
Time Zones -24 time zones -15 degrees inbetween each longitude of time zone
Why are there seasons? due to earths tilt with respect to the sun, and the plane of ecliptic
Equinox subsolar point at equator (SPRING AND FALL)
Solstice subsolar point at tropic of cancer (SUMMER) subsolar point of tropic of capricorn (WINTER)
Electromagnetic Spectrum entire wavelength range of electromagnetic energy
Shortwave sun gives off -emitted by hot objects ex/gamma rays, x-rays, ultraviolet rays, visible light, etc.
Longwave earth gives off -emitted by cooler object ex/thermal infrared part of spectrum
Constant Gas nitrogen, oxygen, and argon
Variable Gas differ in proportion over time and space -make up less than 1% water vapor, ozone
Green House Effect counter radiation is reflected back onto earths surface
Ozone occurs in 2 layers; stratosphere-UV absorbing layer ground level-pollution forms when gaseous chemicals react in upper atmosphere
Particulates needed for rain and cloud formation -liquid form: clouds and rain -solid form: snow, hail, pollutants, soil (dust), smoke, ash, pollen, salt spray
Radiation creation and emission of electromagnetic waves
Conduction involves diffusion of heat through contact
Convection involves upward movement of heat, cold to the bottom, heat to the top
Direct Radiation uninterrupted flow of incoming radiation that reach earth; amount to 25% -remaining 75% absorbed or redirected
Indirect Radiation redirected downward toward surface
Troposphere closest to earths surface heated by longwave radiation; produced by earth
Stratosphere second closest to earth ozone layer
Mesosphere third closest to earths surface Meteor location
Thermosphere farthest from earths surface heated by the sun
Global Radiation Budget balance between incoming (shortwave) radiation and outgoing (longwave) radiation
Net Radiation differance between incoming and outgoing radiation values
Albedo amount of reflection a given surface can course
Mercator Projection corrects relative shape of landmasses -distorts poles -lines of latitude at right angles
Albers Equal Area corrects the relative area of landmasses -distorts shape of landmasses near poles and equator -lines of latitude and longitude are curved
Spatial Analysis attempts to explain patterns or distributions of specific variables over physical space
Physical Geography Process refers to series of actions that can be measured and can produce predictable end result
Longitude Referance Point greenwhich, England
Remote Sensing measure property of enviroment withouth direct contact (aerial photos)
Earths Orbit around the sun counter clockwise
Solar Noon suns highest position
Celestial Dome shows suns daily arc and seasonal migration relative to earths surface
Counterradiation atomosphere redirects some longwave energy back to surface
Sensible Heat can be sensed and measured
Latent Heat is hidden and cannot be measured
Created by: nicolepapageorge
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