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Geog 308 test 1

Megan Bender Inglês 44 flashcards

Flashcards do conjunto (44)

  1. 1the plan1980s
    montreal protocol
    dominant assumptions which frame the problem of CC and offer the solution
    knowledge > action > change
    Problems: not linear, politics and sci dont align, econ interest, understanding pluralistic, disinfo compaigns, not rational
  2. 2pluralistic framingmarket failure
    tech hazard
    global injustice
    overconsumption
    mostly natural
    tipping point
  3. 3system, why do we careset of things that're connected to eachother,
    understand implications of decisions, lag time, reach thresholds or see abrupt changes
  4. 4stocka store, amount, built up over time, snapshot of time,
    accumulations of flows
  5. 5flowrate at which something adds/subtracts something from a stock, measure of time
  6. 6feedbacksamplifying- flow affects stock in a way that makes effect stronger
    stabilizing- feedback acts to bring the system back to a new equilibrium
  7. 7climate variabilityvariations in the mean state/stats of climate on all temporal and spatial scales
  8. 8Climate changestatistically significant variation in the mean persisting for an extended period
  9. 9AtmosphereCO2, water vapor, methane, oxides of N, Ozone
    have sig impact on earths climate and weather
  10. 10water vapormost important GHG, most abundant
    natural GH effect
    varies
    doesnt accumulate, doesnt change concentrations, short life
  11. 11CO2respiration/volcanoes/decay/combustion
    photosynthesis/seasonal variations
    reserves, exchange rates, net changes
  12. 12ozone15-50km up,
    troposphere- created naturally and by photochem reactions, in high concentrations is harmful, minor GHG,
    stratosphere- interaction btwn UV and molecular oxygen
    depletion of good oxygen- absorbs most UV, has holes, CFCs and Halons
  13. 13groundlevel ozonefrom human made emissions,
    causes respiration problems and plant damage
  14. 14methanevariable gas, increasing,
    effective absorber of terrestrial radiation
    released through fossil fuel actvity
  15. 15structure of atmosphere, thermal layerstroposphere warms and cools to stratosphere which warms bc ozone, mesosphere cools, thermosphere warms bc absorbs extreme UV
    troposphere- 80% atmosphere mass, weather, breathable, tropopause changes
  16. 16solar insolationamount of electromagnetic energy that reaches the surface of earth,
    primary heat source,
    most gases in atompshere transparent to
  17. 17global energy budgetbalance btwn incoming solar radiation, absorption of terrestrial radiation, and outgoing radiation (solar and terrestrial)
  18. 18solar radiationradiation emitted by sun, changes by 7% annually,
  19. 19albedofraction of solar radiation reflected by a surface
  20. 20greenhouse effectthe heating of the surface due to the presence of atmosphere contained gases that absorb and emit longwave radiation
  21. 21radiative forcinga measure of the influence that a climate factor has in altering the balance of energy
  22. 22climate warmingenhanced GH effect and positive radiative forcing
  23. 23latitudinal energy balanceradiative equilibrium varies by lat.,
    concentrated near equator,
    net surplus at equator, net deficit at poles, air movement creates ocean and wind currents
  24. 24atmospheric circulationstemp and pressure differnces cause large scale horiz energy transfer throug avection,
    3 cell model
  25. 253 cell modelhadley cells- tropics air heated and diverges when expanded, strength increases during cold season with thermal contrasts maximized,
    polar cells- very cold temps, dense air resulting in sinking and high pressure, warmer air pulled aloft to replace it
    ferrel cells- lie btwn, dependent on air movement
  26. 26Global thermohaline circulationsurface currents forced by friction btwn ocean and wind, ind imparts momentum on ocean,
    heat distribution,
    density driven circulation caused by diff temps and salinity
  27. 27global warming potentiala measure of how much energy a gas traps in atmosphere relative to CO2,
    depends on absorption of IR, which wavelengths absorbed, lifetime
  28. 28forcing mechanismsa process that alters the energy balance,
    solar output, earths orbit, atmospheric composition, tectonics
  29. 29variations in solar outputwarmer in past bc GH effect,
    solar output regularly changes bc sunspots,
    during high freq times of sun spots solar radiation decreases
  30. 30changes in earths orbiteccentricity- shape of orbit changes 100000yrs 1-11%,
    precision of equinox- axis of rotation changes 27000yr cycle alternating timing and intensity of seasons,
    obliquity- earths wobble on axis/tilt, 41000yr, 22.1-24.5 degrees
    (milankovitch cycles)
  31. 31changes in atmospheric compositionaerosols- human and natural, affect absorption/transmission/reflection of insolation and terr. radiation and energy balance
    strat. aerosols smaller and stable conditions so reside longer,
    GHGs
  32. 32changes in land configuration and surface characteristicsposition of land effects absorption, radiation,
    continental drift- veg and ice formation,
    tectonics through mountains and volcanoes
  33. 33geoengineeringdeliberate manipulation of earth to counteract CC, mitigation
  34. 34natural processesphotosynthesis,
    respiration and decay,
    atmos exchange with oceans,
    geologic processes (volcanoes, weathering of rocks take CO2 out of atmosphere)
  35. 35global greenhouse emissions highest sectorsheat/electricity
    transportation
    industrial
    agri and land use change
  36. 36geog of emissionshighest for china, india, US and russia
  37. 37total emissionshighest for china, US, india, russia
  38. 38total emissions per capitahighest for canada, US, australia (smaller population with lots of land)
  39. 39fingerprintsincreased industrial C,
    less heat escaping, more returning,
    oceans warming,
    nights and winters warming,
    stratosphere cooling,
    climate models and emissions to explain warming
  40. 40Fouriercolder if lacked atmosphere, natural green house effect, 1824
  41. 41tyndallgases have varied capacities to absorb/transmit radiant heat,
    change in concentration changes climate
    1850s
  42. 42arrheniushot house theory,
    global warming from human caused CO2 emissions, 1896
  43. 43keelingmeasure of atmosphere CO2,
    upward trend,
    keeling curve,
    1960s
  44. 44nature perspectivescapricious- resource lottery, not controlable, cope
    perverse- unstable, resources scarce, controlable, regulation
    benign- stable, resources abundant
    egalitarian- precarious balance, resources depleting

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FlashCards sobre Geog 308 test 1, criado por Megan Bender em 05-10-2015.
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