1-4feetHow muchthe sea levelcould rise by2100.polarclimatezonehighpressure,sea ice mostof the yearmethaneproducedfromlandfillsand cattleclimatelong-term averageof weather,includesprecipitation andtemperatureCO2product ofburningfossilfuelsExospheremostlyhydrogen,weathersatellites arehereIonosphereconductselectricityand theauroras formherethermosphereWhere theHubbleand ISSorbitweatherconditions ofthe atmosphereat a particulartime and placeProxydataindirectevidenceMilankovitchTheoriesEccentricity,obliquity,andPrecessionPaleoclimatologythe studyof ancientclimateshydrosphereall theliquidwater onEarthcoal, oil,naturalgassourcesof CO2glacial retreat,decreased snowcover, shrinkingice sheet,extreme evertsevidenceof climatechangeatmosphereextends fromthe groundup and intospacegreenhouseeffectwhen gases inthe atmospheretrap heatenergy from thesunGlacialiceringsused todetermineclimate of thepast includingCO2 levelsbiosphereall thelivingthings onearthgeosphere interiorandexterior ofEarthoceanacidificationWhen thereis too muchCO2 in theocean.cryosphereall thefrozenwater onEarthdoldrumsno wind,happens intheequatorialclimate zoneequatorialclimatezonerising airanddoldrumswatervapor66-85% ofgreenhouseeffectstratospherecontainsthe ozonelayer1-4feetHow muchthe sea levelcould rise by2100.polarclimatezonehighpressure,sea ice mostof the yearmethaneproducedfromlandfillsand cattleclimatelong-term averageof weather,includesprecipitation andtemperatureCO2product ofburningfossilfuelsExospheremostlyhydrogen,weathersatellites arehereIonosphereconductselectricityand theauroras formherethermosphereWhere theHubbleand ISSorbitweatherconditions ofthe atmosphereat a particulartime and placeProxydataindirectevidenceMilankovitchTheoriesEccentricity,obliquity,andPrecessionPaleoclimatologythe studyof ancientclimateshydrosphereall theliquidwater onEarthcoal, oil,naturalgassourcesof CO2glacial retreat,decreased snowcover, shrinkingice sheet,extreme evertsevidenceof climatechangeatmosphereextends fromthe groundup and intospacegreenhouseeffectwhen gases inthe atmospheretrap heatenergy from thesunGlacialiceringsused todetermineclimate of thepast includingCO2 levelsbiosphereall thelivingthings onearthgeosphere interiorandexterior ofEarthoceanacidificationWhen thereis too muchCO2 in theocean.cryosphereall thefrozenwater onEarthdoldrumsno wind,happens intheequatorialclimate zoneequatorialclimatezonerising airanddoldrumswatervapor66-85% ofgreenhouseeffectstratospherecontainsthe 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. How much the sea level could rise by 2100.
    1-4 feet
  2. high pressure, sea ice most of the year
    polar climate zone
  3. produced from landfills and cattle
    methane
  4. long-term average of weather, includes precipitation and temperature
    climate
  5. product of burning fossil fuels
    CO2
  6. mostly hydrogen, weather satellites are here
    Exosphere
  7. conducts electricity and the auroras form here
    Ionosphere
  8. Where the Hubble and ISS orbit
    thermosphere
  9. conditions of the atmosphere at a particular time and place
    weather
  10. indirect evidence
    Proxy data
  11. Eccentricity, obliquity, and Precession
    Milankovitch Theories
  12. the study of ancient climates
    Paleoclimatology
  13. all the liquid water on Earth
    hydrosphere
  14. sources of CO2
    coal, oil, natural gas
  15. evidence of climate change
    glacial retreat, decreased snow cover, shrinking ice sheet, extreme everts
  16. extends from the ground up and into space
    atmosphere
  17. when gases in the atmosphere trap heat energy from the sun
    greenhouse effect
  18. used to determine climate of the past including CO2 levels
    Glacial ice rings
  19. all the living things on earth
    biosphere
  20. interior and exterior of Earth
    geosphere
  21. When there is too much CO2 in the ocean.
    ocean acidification
  22. all the frozen water on Earth
    cryosphere
  23. no wind, happens in the equatorial climate zone
    doldrums
  24. rising air and doldrums
    equatorial climate zone
  25. 66-85% of greenhouse effect
    water vapor
  26. contains the ozone layer
    stratosphere