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)?

    • Satellite photos from the 1800s
    • Thermometer readings from millions of years ago
    • Preserved natural records that stand in for direct measurements
    • Forecasts of future weather
  3. Which of these is a proxy record of past climate, by Kira's reading (NOAA)?

    • Tomorrow's forecast
    • Tree rings
    • A modern weather-satellite photo
    • Today's rain-gauge reading
  4. Why do ice cores show yearly layers, by Jun's reading (NOAA)?

    • Summer and winter snow differ in texture and chemistry
    • Layers form from ocean waves
    • Each storm makes one yearly layer
    • Each layer is one century of snow
  5. What do the air bubbles in ice cores hold, by Luz's reading (NOAA)?

    Use the picture in question 3.

    • Ocean water
    • Tree pollen and nothing else
    • Samples of the past atmosphere's gases
    • Modern air pumped in by the drill during coring
  6. 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.

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

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

    • Ten
    • Two, one each season
    • One
    • One per decade
  10. 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 cold, snowy winter
    • A wet year
    • A dry year
  11. What is cross dating, by Ren's reading (NOAA)?

    • 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
    • Matching tree rings to ice layers by color
  12. Use this

    Light oxygen moving from the sea into an ice sheet.

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

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

    • Light oxygen gets locked away in the growing ice sheets
    • The cold ocean makes heavy oxygen
    • Plankton eat the light oxygen
    • Heavy oxygen is locked away in the growing ice sheets there
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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)?

    • Satellite photos from the 1800s
    • Thermometer readings from millions of years ago
    • Preserved natural records that stand in for direct measurements
    • Forecasts of future weather
  3. Which of these is a proxy record of past climate, by Kira's reading (NOAA)?

    • Tomorrow's forecast
    • Tree rings
    • A modern weather-satellite photo
    • Today's rain-gauge reading
  4. Why do ice cores show yearly layers, by Jun's reading (NOAA)?

    • Summer and winter snow differ in texture and chemistry
    • Layers form from ocean waves
    • Each storm makes one yearly layer
    • Each layer is one century of snow
  5. What do the air bubbles in ice cores hold, by Luz's reading (NOAA)?

    Use the picture in question 3.

    • Ocean water
    • Tree pollen and nothing else
    • Samples of the past atmosphere's gases
    • Modern air pumped in by the drill during coring
  6. 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.

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

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

    • Ten
    • Two, one each season
    • One
    • One per decade
  10. 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 cold, snowy winter
    • A wet year
    • A dry year
  11. What is cross dating, by Ren's reading (NOAA)?

    • 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
    • Matching tree rings to ice layers by color
  12. Use this

    Light oxygen moving from the sea into an ice sheet.

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

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

    • Light oxygen gets locked away in the growing ice sheets
    • The cold ocean makes heavy oxygen
    • Plankton eat the light oxygen
    • Heavy oxygen is locked away in the growing ice sheets there