oceanacidificationWhen thereis too muchCO2 in theocean.coal, oil,naturalgassourcesof CO2methaneproducedfromlandfillsand cattlethermosphereWhere theHubbleand ISSorbitIonosphereconductselectricityand theauroras formhereCO2product ofburningfossilfuelsequatorialclimatezonerising airanddoldrumsgeosphere interiorandexterior ofEarthgreenhouseeffectwhen gases inthe atmospheretrap heatenergy from thesunweatherconditions ofthe atmosphereat a particulartime and placeglacial retreat,decreased snowcover, shrinkingice sheet,extreme evertsevidenceof climatechangeMilankovitchTheoriesEccentricity,obliquity,andPrecessionProxydataindirectevidencehydrosphereall theliquidwater onEarthpolarclimatezonehighpressure,sea ice mostof the yeardoldrumsno wind,happens intheequatorialclimate zoneGlacialiceringsused todetermineclimate of thepast includingCO2 levelsPaleoclimatologythe studyof ancientclimateswatervapor66-85% ofgreenhouseeffect1-4feetHow muchthe sea levelcould rise by2100.climatelong-term averageof weather,includesprecipitation andtemperaturebiosphereall thelivingthings onearthatmosphereextends fromthe groundup and intospaceExospheremostlyhydrogen,weathersatellites areherecryosphereall thefrozenwater onEarthstratospherecontainsthe ozonelayeroceanacidificationWhen thereis too muchCO2 in theocean.coal, oil,naturalgassourcesof CO2methaneproducedfromlandfillsand cattlethermosphereWhere theHubbleand ISSorbitIonosphereconductselectricityand theauroras formhereCO2product ofburningfossilfuelsequatorialclimatezonerising airanddoldrumsgeosphere interiorandexterior ofEarthgreenhouseeffectwhen gases inthe atmospheretrap heatenergy from thesunweatherconditions ofthe atmosphereat a particulartime and placeglacial retreat,decreased snowcover, shrinkingice sheet,extreme evertsevidenceof climatechangeMilankovitchTheoriesEccentricity,obliquity,andPrecessionProxydataindirectevidencehydrosphereall theliquidwater onEarthpolarclimatezonehighpressure,sea ice mostof the yeardoldrumsno wind,happens intheequatorialclimate zoneGlacialiceringsused todetermineclimate of thepast includingCO2 levelsPaleoclimatologythe studyof ancientclimateswatervapor66-85% ofgreenhouseeffect1-4feetHow muchthe sea levelcould rise by2100.climatelong-term averageof weather,includesprecipitation andtemperaturebiosphereall thelivingthings onearthatmosphereextends fromthe groundup and intospaceExospheremostlyhydrogen,weathersatellites areherecryosphereall thefrozenwater onEarthstratospherecontainsthe ozonelayer

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