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The study of natural systems (processes), geographic areas, society and their interdependece over space. |
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What are the 5 major spatial themes? |
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Location, region, human-earth relations, movement, place |
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integration of all things, systems theory |
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-Shows interrelationships between objects and processes -contains inputs, outputs, processes, feedbacks, etc -open and closed systems |
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-flows of energy and mass -a river |
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-energy flows into a system and energy flows out -not self-sustaining -earths energy budget(example) |
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-a system that is shut off from surrounding environment so that it is self contained -Earths mass budget |
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-maintence of structure and character over time -no large changes |
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-changing trend over time |
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What happens when a system reaches a threashold? |
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-metastable equillibrium -abrupt change-can't ever go back |
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-enchances change in a system -creates runaway/snowball effect |
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example of positive feedback |
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-diminishes change in a systed -causes self-regulation -info discourages response in a system |
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example of negative feedback |
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bad review affecting ticket sales |
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What are the 4 major spheres? |
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-atmosphere -lithosphere -hydroshphere -biosphere |
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thin gaseous veil surrounding earth |
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water in 3 phases found in earth |
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earths crust and upper mantle (rocks) |
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interconected web that links all organizms with their physical environment |
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measurement of electromagentic radiation reflected or emitted form remote bodies |
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-human eyes can see -shows clouds -only certain times and loacatios when it can be used |
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more descriptice reading of clouds longer wavelenghts |
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records energy radiated or refelected form a surface |
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examples of passive remote sensing |
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-visable light -emitting of human radiation -human eyes |
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sends radiation and records reflection |
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examples of active remote sensing |
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radar microwaves wavelenghts/radiation |
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electromagnetic radiation |
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emitted from all bodies above 0 Kelvins (absolute zero) travels at speed of light(in a vacuum) |
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all objects radiate energy at wavelenths's inversly proportional to their temperature |
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major reasons for the seasons |
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changes in day length and the suns altitude above the horizon over the course of the year |
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The moment when the Sun is positioned directly over the Earth's equator and, by extension, the apparent position of the Sun at that moment |
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occurs around December 21 or 22 each year in the Northern hemisphere, and June 21 or 22 in the Southern Hemisphere. It is on the shortest day or longest night of the year |
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longest day shortest night |
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major bands of radiation emitted by the sun |
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-ultraviolet -x-ray -gamma ray wavelenghts -visbale light -infared |
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what band is the solar peak? |
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-warm air over cold air -stable atmosphere -no mixing -flat |
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-mixing in the atmosphere -creates a lot of instablity |
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natural sources for variable gasses and aerosols |
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volcanic erruptions dust storms pollens/spores salt crystals (oceans) |
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anthropogenci reasons for variable gasses and aerosols |
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nuclear weaspons industrial pollution |
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natural factors of air pollution |
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winds local topography temperature inversions |
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anthropogenic factors for air pollution |
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carbon monoxide emmissions photo-chemical smog |
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some energy is absorbed by the atmosphere and then radiated as longwave radiation |
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-from ground or atmosphere back to space -a funciton of albedo |
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the atmosphere is transparent to shortwave radiation but absorbs longwave radiation --hence heat is stored in teh atmosphere |
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other methods of heat transport besides radiation |
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convection conduction advection |
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molecule to molecule transfer of heat energy warm to cool |
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temp. differences between land and water bodies soil temp. |
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gasses and liquids only strong vertical motion
--atmospheric and oceanic circulations --weather systems |
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horizontal motion warmer masses(less dense) rise and cooler(denser)tend to sink
--horizontal movement of winds from land to sea --movement of fog |
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what controls spatial patterns of temperatre |
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latitdude altidtude albedo clouds water |
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latitudes effects on temperature |
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-lower latitude = less change in seasons -higher = greater range -high lat = cold avg. temp -low lat. = warm avg. temp -effects insolation |
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cloud cover's effect on temp during day |
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reduces insolation therfore reduces temperatre |
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cloud cover's effect on temp during night |
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reduces longwave radiation which means higher temp clouds moderate temp |
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land-water heating differnces effects on temp |
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water = mixing land = no mixing evaporation, transparent, specific heat capacity, movement |
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rolse of water on average temp. |
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role of water on avg range |
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larger range further away from water bodies |
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the energy is stored in water vapor, released when it condences |
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more dense higher pressure poles |
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less dense lower pressure equator |
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from high to low pressure |
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closer isobars stronger winds |
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caused by earths rotation causes air to curve -right in n.hem and left in s.hem -strongest at poles -0 at the equator |
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friction near surface causes air to spiral slows down-reduces coriolis force slows down wind opposite and proportional to the force |
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ascending air clouds, percipitation, stronger winds hurricanes |
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descedning air clear skies, weak winds spirals out near surface |
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equatorial low pressure system |
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warm and wet generated by thermal factors |
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polar high pressure system |
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cold and dry thermal factors |
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sub-tropical high pressure |
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descdeing air hot and dry (desert and higest max temp) dynamic factors warm air from tropics moves to cold air(cold current) medeterannien |
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sub-polar low pressure system |
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cool and wet dynamic advection uplift of warmer aire/cold air down |
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low pressure warm, moist rising air, clouds and rain, moonsoon, high rainfall. |
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develop in the tropics spiral opp. directions in diff hemispheres needs lots of warm water and h20 evaporation hast to be 5 degrees north or south of equator for corolis force to work domes up at trophopause |
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cold air and warm air mixing cloud development |
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cold air coming into a warmer region cold crisp days after rain |
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warm air moving into a cold region gentle lifting more layered clouds |
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surface winds, oceanic temp and salinity gradients with corilois force eaporation leaves salt therfore more dense versus fresh h20 |
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sea to land isobars far apart high pressure systems |
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ratio of water vapor content to maximum water vapor capacity |
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actual amount of water vapor in teh atmosphere |
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the maximum amount of water vapor an airmass can hold before it becomes saturated and condenses
function of temperature only |
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increase in water vapor decrease in temperatre |
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form when air gets saturated and conensations occurs form form air cooling due to rising |
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any cloud in contact with the ground |
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relatively warm and moist air from the pacific crosses the cold californinan current |
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cold air draigage in valleys |
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suface cooling surface radiation budget in deficet typically nights and winters |
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