Climate change at the poles · seed 1 · A4, ink-friendly. The answer key prints on its own page for grown-ups.
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The poles are warming up

Science · Polar Regions · ages 9-11
Name ______________________   Date ____________
  1. In the ice-albedo feedback, what happens when sea ice melts away?

    • The ocean immediately becomes covered by thicker ice.
    • More dark ocean is exposed to sunlight.
    • The exposed ocean reflects all sunlight into space.
  2. Which comparison helps scientists track long-term change in late-summer Arctic sea ice?

    • September sea ice extent across many years
    • January and September sea ice extent in just one year
    • Morning and evening air temperatures on just one day
  3. Ice lost from Greenland and Antarctica's land-based ice sheets can enter the ocean and raise sea level.

    Circle one:   True   False

  4. A made-up practice model starts with 100 ice units. Remove 13 units for one decade and 13 more for another. How many units remain? This model is not satellite data.

    Answer: ______________

  5. Dark ocean absorbs extra sunlight as heat after sea ice melts. How can this affect nearby sea ice?

    • It always freezes all nearby ocean water.
    • It has no effect on any nearby sea ice.
    • It can melt more nearby sea ice.
  6. Microbes in wet, thawed ground can release methane. Why can this add to climate warming?

    • Methane slows the escape of some heat to space.
    • Methane reflects all incoming sunlight back into space.
    • Methane stops all sunlight from reaching ocean water.
  7. Which chain describes a permafrost feedback in which the first warming leads to more warming?

    • Warming thaws ground, gases cool the air, and the ground freezes.
    • Warming thaws ground, plant matter stays frozen, and gases vanish.
    • Warming thaws ground, gases slow heat loss, and more ground thaws.
  8. One September has more Arctic sea ice than the September before it. A student says this proves the long-term decline has ended. Which explanation checks that claim?

    • One year's increase proves the Arctic's long-term decline has ended.
    • One year's increase can occur during a long-term decline.
    • One year's increase shows all earlier satellite measurements were false.
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Answer key

For grown-ups. Fold this page away before handing over the rest.

The poles are warming up W1-mt_Fqna9qHffr-s1

  1. More dark ocean is exposed to sunlight. · Sea-ice loss exposes darker ocean water, which absorbs more sunlight than white sea ice.
  2. September sea ice extent across many years · Comparing September extent across many years tracks long-term change while keeping the season the same.
  3. True · These ice sheets store water on land. Losing that ice to the ocean adds water and raises sea level.
  4. 74 · Subtract both losses: 100 - 13 - 13 = 74 units. This follows the stated practice model, not an observed rate.
  5. It can melt more nearby sea ice. · The extra absorbed energy warms the ocean and can help melt more nearby sea ice.
  6. Methane slows the escape of some heat to space. · Methane is a greenhouse gas. It absorbs some heat energy Earth gives off and slows heat loss to space.
  7. Warming thaws ground, gases slow heat loss, and more ground thaws. · Thawing can release greenhouse gases. Their warming effect can cause more thawing, strengthening the starting change.
  8. One year's increase can occur during a long-term decline. · Individual years vary. One increase does not show that a trend measured over many decades has ended.
Worksheet · LightMySky