climatelong-term averageof weather,includesprecipitation andtemperatureatmosphereextends fromthe groundup and intospacethermosphereWhere theHubbleand ISSorbitglacial retreat,decreased snowcover, shrinkingice sheet,extreme evertsevidenceof climatechangecryosphereall thefrozenwater onEarthweatherconditions ofthe atmosphereat a particulartime and placeExospheremostlyhydrogen,weathersatellites areherecoal, oil,naturalgassourcesof CO2greenhouseeffectwhen gases inthe atmospheretrap heatenergy from thesundoldrumsno wind,happens intheequatorialclimate zonepolarclimatezonehighpressure,sea ice mostof the yearmethaneproducedfromlandfillsand cattleProxydataindirectevidencestratospherecontainsthe ozonelayerMilankovitchTheoriesEccentricity,obliquity,andPrecessionIonosphereconductselectricityand theauroras formhereoceanacidificationWhen thereis too muchCO2 in theocean.biosphereall thelivingthings onearthhydrosphereall theliquidwater onEarthwatervapor66-85% ofgreenhouseeffectGlacialiceringsused todetermineclimate of thepast includingCO2 levels1-4feetHow muchthe sea levelcould rise by2100.equatorialclimatezonerising airanddoldrumsPaleoclimatologythe studyof ancientclimatesCO2product ofburningfossilfuelsgeosphere interiorandexterior ofEarthclimatelong-term averageof weather,includesprecipitation andtemperatureatmosphereextends fromthe groundup and intospacethermosphereWhere theHubbleand ISSorbitglacial retreat,decreased snowcover, shrinkingice sheet,extreme evertsevidenceof climatechangecryosphereall thefrozenwater onEarthweatherconditions ofthe atmosphereat a particulartime and placeExospheremostlyhydrogen,weathersatellites areherecoal, oil,naturalgassourcesof CO2greenhouseeffectwhen gases inthe atmospheretrap heatenergy from thesundoldrumsno wind,happens intheequatorialclimate zonepolarclimatezonehighpressure,sea ice mostof the yearmethaneproducedfromlandfillsand cattleProxydataindirectevidencestratospherecontainsthe ozonelayerMilankovitchTheoriesEccentricity,obliquity,andPrecessionIonosphereconductselectricityand theauroras formhereoceanacidificationWhen thereis too muchCO2 in theocean.biosphereall thelivingthings onearthhydrosphereall theliquidwater onEarthwatervapor66-85% ofgreenhouseeffectGlacialiceringsused todetermineclimate of thepast includingCO2 levels1-4feetHow muchthe sea levelcould rise by2100.equatorialclimatezonerising airanddoldrumsPaleoclimatologythe studyof ancientclimatesCO2product ofburningfossilfuelsgeosphere interiorandexterior ofEarth

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