A blue Antarctic glacier wall reflected in ocean water

Chapter 3 · Grades 4–6

A changing Antarctica

What happens in Antarctica does not stay in Antarctica. Its ice, ocean, and wildlife are connected to the whole planet.

Antarctic glacier wall · WindWalker Antarctic photo archive

First, the big idea

Earth is warming because people have added extra heat-trapping gases to the atmosphere.

Burning coal, oil, and gas releases carbon dioxide. This gas acts a little like an extra blanket around Earth. As air and oceans warm, Antarctica’s ice and living systems respond.

Four connected changes

Ice, ocean, animals, people

A change in one part of the Antarctic system can travel through the others.

Land ice loses mass

Satellites show that Antarctica’s ice sheet has been losing ice overall since measurements began in 2002. When land ice reaches the ocean, global sea level rises.

Sea ice habitat shifts

Sea ice freezes ocean water and floats. Its timing, thickness, and area affect algae, young krill, penguins, seals, and the animals that eat them.

The ocean changes

The Southern Ocean is warming in many places. It also absorbs carbon dioxide, which makes the water more acidic and can make life harder for some organisms.

The food web feels it

Young krill shelter and feed beneath sea ice. Changes to krill can ripple outward to fish, penguins, seals, seabirds, and whales.

Animals must adjust

Some penguin colonies may have to travel farther to reach food or find stable ice. Species do not all respond in the same way.

Coasts far away are linked

Added water from melting land ice raises sea level around the world, increasing risks for people and habitats near coastlines.

An Antarctic iceberg arch meeting the dark ocean water
An iceberg is floating ice. The huge ice sheet rests on land.

Words that matter

Not all ice is the same

Land ice is snow and ice piled on the continent. When it melts or flows into the ocean, it adds water and raises sea level.

Sea ice forms when ocean water freezes. It already floats, so melting it does not directly raise sea level—just as melting ice cubes do not overflow a full glass. But sea ice is vital habitat and helps reflect sunlight.

How do scientists know?

Satellites measure the height, area, and mass of ice. Weather stations record air conditions. Ships, floats, and instruments carried by seals measure the ocean. Biologists count animals and follow where they feed. One measurement is a clue; many measurements over time reveal a pattern.

Think like a scientist

Ask careful questions

Climate science is not about one hot day or one snowy week. It is about gathering evidence, comparing years, checking ideas, and being honest about what we still need to learn.

  • How was this measured?
  • Is it weather or a long-term climate pattern?
  • Does the same change happen everywhere?
  • What other evidence supports the idea?

Reasons for hope

Knowledge helps people act

Countries protect Antarctica through international agreements, and researchers share discoveries across borders. Children can help by learning, asking good questions, caring for energy and materials, and sharing accurate science. Big climate solutions also need communities, scientists, companies, and governments working together.

Science sources

This chapter was checked against current educational and satellite-based information from NASA and the Australian Antarctic Program.