coal, oil,naturalgassourcesof CO2oceanacidificationWhen thereis too muchCO2 in theocean.MilankovitchTheoriesEccentricity,obliquity,andPrecessionGlacialiceringsused todetermineclimate of thepast includingCO2 levelsclimatelong-term averageof weather,includesprecipitation andtemperaturewatervapor66-85% ofgreenhouseeffectdoldrumsno wind,happens intheequatorialclimate zonePaleoclimatologythe studyof ancientclimatesgreenhouseeffectwhen gases inthe atmospheretrap heatenergy from thesunmethaneproducedfromlandfillsand cattlecryosphereall thefrozenwater onEarthCO2product ofburningfossilfuelsstratospherecontainsthe ozonelayerequatorialclimatezonerising airanddoldrumsthermosphereWhere theHubbleand ISSorbitbiosphereall thelivingthings onearthatmosphereextends fromthe groundup and intospacepolarclimatezonehighpressure,sea ice mostof the yearhydrosphereall theliquidwater onEarthExospheremostlyhydrogen,weathersatellites arehereIonosphereconductselectricityand theauroras formhereglacial retreat,decreased snowcover, shrinkingice sheet,extreme evertsevidenceof climatechange1-4feetHow muchthe sea levelcould rise by2100.geosphere interiorandexterior ofEarthweatherconditions ofthe atmosphereat a particulartime and placeProxydataindirectevidencecoal, oil,naturalgassourcesof CO2oceanacidificationWhen thereis too muchCO2 in theocean.MilankovitchTheoriesEccentricity,obliquity,andPrecessionGlacialiceringsused todetermineclimate of thepast includingCO2 levelsclimatelong-term averageof weather,includesprecipitation andtemperaturewatervapor66-85% ofgreenhouseeffectdoldrumsno wind,happens intheequatorialclimate zonePaleoclimatologythe studyof ancientclimatesgreenhouseeffectwhen gases inthe atmospheretrap heatenergy from thesunmethaneproducedfromlandfillsand cattlecryosphereall thefrozenwater onEarthCO2product ofburningfossilfuelsstratospherecontainsthe ozonelayerequatorialclimatezonerising airanddoldrumsthermosphereWhere theHubbleand ISSorbitbiosphereall thelivingthings onearthatmosphereextends fromthe groundup and intospacepolarclimatezonehighpressure,sea ice mostof the yearhydrosphereall theliquidwater onEarthExospheremostlyhydrogen,weathersatellites arehereIonosphereconductselectricityand theauroras formhereglacial retreat,decreased snowcover, shrinkingice sheet,extreme evertsevidenceof climatechange1-4feetHow muchthe sea levelcould rise by2100.geosphere interiorandexterior ofEarthweatherconditions ofthe atmosphereat a particulartime and placeProxydataindirectevidence

Climate Bingo - Call List

(Print) Use this randomly generated list as your call list when playing the game. There is no need to say the BINGO column name. Place some kind of mark (like an X, a checkmark, a dot, tally mark, etc) on each cell as you announce it, to keep track. You can also cut out each item, place them in a bag and pull words from the bag.


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  1. sources of CO2
    coal, oil, natural gas
  2. When there is too much CO2 in the ocean.
    ocean acidification
  3. Eccentricity, obliquity, and Precession
    Milankovitch Theories
  4. used to determine climate of the past including CO2 levels
    Glacial ice rings
  5. long-term average of weather, includes precipitation and temperature
    climate
  6. 66-85% of greenhouse effect
    water vapor
  7. no wind, happens in the equatorial climate zone
    doldrums
  8. the study of ancient climates
    Paleoclimatology
  9. when gases in the atmosphere trap heat energy from the sun
    greenhouse effect
  10. produced from landfills and cattle
    methane
  11. all the frozen water on Earth
    cryosphere
  12. product of burning fossil fuels
    CO2
  13. contains the ozone layer
    stratosphere
  14. rising air and doldrums
    equatorial climate zone
  15. Where the Hubble and ISS orbit
    thermosphere
  16. all the living things on earth
    biosphere
  17. extends from the ground up and into space
    atmosphere
  18. high pressure, sea ice most of the year
    polar climate zone
  19. all the liquid water on Earth
    hydrosphere
  20. mostly hydrogen, weather satellites are here
    Exosphere
  21. conducts electricity and the auroras form here
    Ionosphere
  22. evidence of climate change
    glacial retreat, decreased snow cover, shrinking ice sheet, extreme everts
  23. How much the sea level could rise by 2100.
    1-4 feet
  24. interior and exterior of Earth
    geosphere
  25. conditions of the atmosphere at a particular time and place
    weather
  26. indirect evidence
    Proxy data