How we know past climates: ice cores, tree rings, sediments

Grade 9 Science Worksheet - Building Confidence

NameDate

Circle the best answer.

  1. Read this first

    Use this

    Ice, a tree ring, a sediment layer and a pollen grain in a row.

  2. What are proxy data, by Ari's reading (NOAA)?

    • Forecasts of future weather
    • Thermometer readings from millions of years ago
    • Satellite photos from the 1800s
    • Preserved natural records that stand in for direct measurements
  3. Why do scientists need proxy data, by Bo's reading (NOAA)?

    • Thermometers have recorded millions of years
    • Satellites have watched for 1,000 years
    • Weather does not change over time
    • Instrument records reach back only to about the 1800s
  4. Why do ice cores show yearly layers, by Jun's reading (NOAA)?

    • Summer and winter snow differ in texture and chemistry
    • Each layer is one century of snow
    • Each storm makes one yearly layer
    • Layers form from ocean waves
  5. Use this

    Table, Ice-core CO₂ and Antarctic temperature (NOAA NCEI), with columns About how long ago, CO₂ in trapped air (ppm), Temperature vs last 1,000 years: 20,000 years, 194, −9.4 °C; 128,000 years, 276, +3.4 °C; 140,000 years, 193, −9.1 °C. Note: CO₂: Antarctic composite (Bereiter et al. 2015); temperature: EPICA Dome C (Jouzel et al. 2007); values rounded.

  6. Using the ice-core table, how much CO₂ did trapped air hold about 20,000 years ago, near the last ice age's peak, by Milo's reading (NOAA)?

    • About 194 ppm
    • About 276 ppm
    • About 425 ppm
    • About 9.4 ppm
  7. Ring widths of a rain-sensitive tree (model data)

    YearRing width
    19013 mm
    19021 mm
    19034 mm
  8. In temperate regions, how many rings does a tree usually add each year, by Noah's reading (NOAA)?

    • One per decade
    • Ten
    • Two, one each season
    • One
  9. A tree depends on rain in its growing season. What does a wide ring show, by Pia's reading (NOAA)?

    • A year when the tree did not grow
    • A wet year
    • A cold, snowy winter
    • A dry year
  10. What is cross dating, by Ren's reading (NOAA)?

    • Matching tree rings to ice layers by color
    • Measuring the height of a tree
    • Counting the rings on a single stump by itself
    • Matching ring patterns in old wood to living trees to fix exact years
  11. Use this

    Light oxygen moving from the sea into an ice sheet.

  12. Oxygen comes in light (oxygen-16) and heavy (oxygen-18) forms. Which evaporates slightly more easily, by Tala's reading (NASA)?

    • Light oxygen-16
    • Neither one evaporates
    • They evaporate equally
    • Heavy oxygen-18
  13. During ice ages, why is the ocean richer in heavy oxygen, by Zee's reading (NASA)?

    • The cold ocean makes heavy oxygen
    • Heavy oxygen is locked away in the growing ice sheets there
    • Plankton eat the light oxygen
    • Light oxygen gets locked away in the growing ice sheets
  14. In a polar ice core, one layer holds less heavy oxygen (oxygen-18) than the layers around it. What does that suggest, by Esme's reading (NASA)?

    • Colder conditions when the snow fell
    • Warmer conditions when the snow fell
    • A wet tree-ring year
    • A volcanic eruption
PencilGopencilgo.com

How we know past climates: ice cores, tree rings, sediments

Answer Key - Grade 9 Science Worksheet - Building Confidence

Circle the best answer.

  1. Read this first

    Use this

    Ice, a tree ring, a sediment layer and a pollen grain in a row.

  2. What are proxy data, by Ari's reading (NOAA)?

    • Forecasts of future weather
    • Thermometer readings from millions of years ago
    • Satellite photos from the 1800s
    • Preserved natural records that stand in for direct measurements
  3. Why do scientists need proxy data, by Bo's reading (NOAA)?

    • Thermometers have recorded millions of years
    • Satellites have watched for 1,000 years
    • Weather does not change over time
    • Instrument records reach back only to about the 1800s
  4. Why do ice cores show yearly layers, by Jun's reading (NOAA)?

    • Summer and winter snow differ in texture and chemistry
    • Each layer is one century of snow
    • Each storm makes one yearly layer
    • Layers form from ocean waves
  5. Use this

    Table, Ice-core CO₂ and Antarctic temperature (NOAA NCEI), with columns About how long ago, CO₂ in trapped air (ppm), Temperature vs last 1,000 years: 20,000 years, 194, −9.4 °C; 128,000 years, 276, +3.4 °C; 140,000 years, 193, −9.1 °C. Note: CO₂: Antarctic composite (Bereiter et al. 2015); temperature: EPICA Dome C (Jouzel et al. 2007); values rounded.

  6. Using the ice-core table, how much CO₂ did trapped air hold about 20,000 years ago, near the last ice age's peak, by Milo's reading (NOAA)?

    • About 194 ppm
    • About 276 ppm
    • About 425 ppm
    • About 9.4 ppm
  7. Ring widths of a rain-sensitive tree (model data)

    YearRing width
    19013 mm
    19021 mm
    19034 mm
  8. In temperate regions, how many rings does a tree usually add each year, by Noah's reading (NOAA)?

    • One per decade
    • Ten
    • Two, one each season
    • One
  9. A tree depends on rain in its growing season. What does a wide ring show, by Pia's reading (NOAA)?

    • A year when the tree did not grow
    • A wet year
    • A cold, snowy winter
    • A dry year
  10. What is cross dating, by Ren's reading (NOAA)?

    • Matching tree rings to ice layers by color
    • Measuring the height of a tree
    • Counting the rings on a single stump by itself
    • Matching ring patterns in old wood to living trees to fix exact years
  11. Use this

    Light oxygen moving from the sea into an ice sheet.

  12. Oxygen comes in light (oxygen-16) and heavy (oxygen-18) forms. Which evaporates slightly more easily, by Tala's reading (NASA)?

    • Light oxygen-16
    • Neither one evaporates
    • They evaporate equally
    • Heavy oxygen-18
  13. During ice ages, why is the ocean richer in heavy oxygen, by Zee's reading (NASA)?

    • The cold ocean makes heavy oxygen
    • Heavy oxygen is locked away in the growing ice sheets there
    • Plankton eat the light oxygen
    • Light oxygen gets locked away in the growing ice sheets
  14. In a polar ice core, one layer holds less heavy oxygen (oxygen-18) than the layers around it. What does that suggest, by Esme's reading (NASA)?

    • Colder conditions when the snow fell
    • Warmer conditions when the snow fell
    • A wet tree-ring year
    • A volcanic eruption