Deep ocean currents: cold, salty water sinks

Grade 9 Science Worksheet

NameDate

Circle the best answer.

  1. Read this first

    Water samples (model data)

    SampleTemperatureSalinity
    A2 °C35 g/kg
    B2 °C33 g/kg
    C20 °C35 g/kg
    D20 °C33 g/kg
  2. Using the sample table, which water would stay at the surface, by Esme's reading?

    • D, warm and fresher
    • A, cold and salty
    • B, cold and fresher
    • C, warm and salty
  3. Sea ice forming above saltier, sinking water. NOAA: where the conveyor starts, warm water from the Gulf Stream loses heat to the cold air. What happens to that water, by Jun's reading?

    • It freshens and floats
    • It cools, grows denser and sinks
    • It warms and rises
    • The wind pushes it to the bottom
  4. Use this

    The global conveyor drawn on a world map.

  5. After sinking in the North Atlantic, which way does the deep water flow, by Kira's reading (NOAA)?

    • Straight up to the surface
    • North, toward the Arctic
    • East, across the Atlantic into a closed inland sea
    • South, past the equator, toward Antarctica
  6. Where do branches of the conveyor rise back toward the surface, by Luz's reading (NOAA)?

    • They stay deep for good
    • Near the poles, where they cool
    • At the conveyor's North Atlantic start, where they cool
    • In the Indian and Pacific Oceans, as they warm
  7. A deep current moves 3 cm a second (example data). How far does it go in one day, by Noah's math?

    • About 72 cm
    • About 260 m
    • About 2.6 km
    • About 26 km
  8. At about 2.6 km a day, about how far does that current go in a year, by Pia's math?

    Use the picture in question 5.

    • About 950 km
    • About 95 km
    • About 2.6 km
    • About 9,500 km
  9. NOAA: a loop takes about 1,000 years. If a parcel covers 60,000 km in that time (example), what is its average speed, by Ren's math?

    • About 60,000,000 km a year
    • About 6 km a year
    • About 60 km a year
    • About 60 km a day
  10. NOAA: wind and tidal currents move tens to hundreds of cm a second. How does a 3 cm/s deep current compare with a 100 cm/s surface current, by Tala's math?

    Use the picture in question 7.

    • The surface current is about 33 times faster
    • The deep current is about 33 times faster
    • They are about equal
    • The surface current is 97 times faster
  11. Wind arrows above, density arrows far below. Which of these currents is driven by density rather than wind, by Zee's reading (NOAA)?

    • Deep water flowing south from the North Atlantic
    • Coastal upwelling
    • The trade-wind drift pushed along near the equator
    • A western boundary current
  12. The global conveyor drawn on a world map. NOAA: warm surface waters are low in nutrients, and deep water in the conveyor is enriched again. Why are upwelling zones rich in algae, by Ari's reading?

    • Sinking water carries algae down
    • Sea ice adds nutrients as it forms
    • Warm surface water holds the most nutrients
    • Rising deep water brings nutrients back to the sunlit surface
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Deep ocean currents: cold, salty water sinks

Answer Key - Grade 9 Science Worksheet

Circle the best answer.

  1. Read this first

    Water samples (model data)

    SampleTemperatureSalinity
    A2 °C35 g/kg
    B2 °C33 g/kg
    C20 °C35 g/kg
    D20 °C33 g/kg
  2. Using the sample table, which water would stay at the surface, by Esme's reading?

    • D, warm and fresher
    • A, cold and salty
    • B, cold and fresher
    • C, warm and salty
  3. Sea ice forming above saltier, sinking water. NOAA: where the conveyor starts, warm water from the Gulf Stream loses heat to the cold air. What happens to that water, by Jun's reading?

    • It freshens and floats
    • It cools, grows denser and sinks
    • It warms and rises
    • The wind pushes it to the bottom
  4. Use this

    The global conveyor drawn on a world map.

  5. After sinking in the North Atlantic, which way does the deep water flow, by Kira's reading (NOAA)?

    • Straight up to the surface
    • North, toward the Arctic
    • East, across the Atlantic into a closed inland sea
    • South, past the equator, toward Antarctica
  6. Where do branches of the conveyor rise back toward the surface, by Luz's reading (NOAA)?

    • They stay deep for good
    • Near the poles, where they cool
    • At the conveyor's North Atlantic start, where they cool
    • In the Indian and Pacific Oceans, as they warm
  7. A deep current moves 3 cm a second (example data). How far does it go in one day, by Noah's math?

    • About 72 cm
    • About 260 m
    • About 2.6 km
    • About 26 km
  8. At about 2.6 km a day, about how far does that current go in a year, by Pia's math?

    Use the picture in question 5.

    • About 950 km
    • About 95 km
    • About 2.6 km
    • About 9,500 km
  9. NOAA: a loop takes about 1,000 years. If a parcel covers 60,000 km in that time (example), what is its average speed, by Ren's math?

    • About 60,000,000 km a year
    • About 6 km a year
    • About 60 km a year
    • About 60 km a day
  10. NOAA: wind and tidal currents move tens to hundreds of cm a second. How does a 3 cm/s deep current compare with a 100 cm/s surface current, by Tala's math?

    Use the picture in question 7.

    • The surface current is about 33 times faster
    • The deep current is about 33 times faster
    • They are about equal
    • The surface current is 97 times faster
  11. Wind arrows above, density arrows far below. Which of these currents is driven by density rather than wind, by Zee's reading (NOAA)?

    • Deep water flowing south from the North Atlantic
    • Coastal upwelling
    • The trade-wind drift pushed along near the equator
    • A western boundary current
  12. The global conveyor drawn on a world map. NOAA: warm surface waters are low in nutrients, and deep water in the conveyor is enriched again. Why are upwelling zones rich in algae, by Ari's reading?

    • Sinking water carries algae down
    • Sea ice adds nutrients as it forms
    • Warm surface water holds the most nutrients
    • Rising deep water brings nutrients back to the sunlit surface