Arctic vs Antarctica: Two Very Different Polar Worlds
Part of Cold Environment Characteristics · GCSE GCSE Geography revision
This deep dive covers Arctic vs Antarctica: Two Very Different Polar Worlds within Cold Environment Characteristics for GCSE Geography. Revise Cold Environment Characteristics in Cold Environments for GCSE Geography with 15 exam-style questions and 20 flashcards. This topic appears regularly enough that it should still be part of a steady revision cycle. It is section 2 of 14 in this topic. Use this deep dive to connect the idea to the wider topic before moving on to questions and flashcards.
Topic position
Section 2 of 14
Practice
15 questions
Recall
20 flashcards
🗺️ Arctic vs Antarctica: Two Very Different Polar Worlds
The first thing to understand about polar environments is that the Arctic and Antarctica are fundamentally different in their physical nature — even though both are cold, icy and at opposite ends of the Earth. Getting this distinction right in an exam is essential.
The Arctic is an ocean — the Arctic Ocean — surrounded by the land masses of Canada, Russia, Greenland, Norway and Alaska. Most of the Arctic's "ice" is sea ice: frozen ocean water, typically 2–4 metres thick. This sea ice floats on the ocean surface, expanding in winter and retreating in summer. Beneath the sea ice there is ocean, not land. The land surrounding the Arctic Ocean is tundra — treeless, permafrost-underlain terrain covered in mosses, lichens and low-growing plants.
Antarctica, by contrast, is a continent — a landmass the size of Europe and the United States combined — surrounded by the Southern Ocean. Antarctica has an ice sheet resting directly on bedrock, up to 4.8 km thick in places. This is not floating sea ice: it is glacial ice built up over hundreds of thousands of years from compacted snow. Antarctica is the coldest, driest, windiest and highest continent on Earth, with an average elevation of 2,300 metres above sea level.
| Feature | Arctic | Antarctica |
|---|---|---|
| Physical nature | Ocean (Arctic Ocean) surrounded by land | Continent (land mass) surrounded by ocean |
| Ice type | Floating sea ice, 2–4 m thick | Ice sheet on bedrock, up to 4.8 km thick |
| Area | ~14 million km² | ~14 million km² |
| Average winter temperature | Around −40°C | Around −60°C (interior plateau) |
| Lowest temperature recorded | −68°C (Siberia, adjacent land) | −89.2°C (Vostok Station, 1983) |
| Wind | Moderate; Arctic storms severe but not extreme | Katabatic winds reach 200 km/h off ice plateau |
| Annual precipitation | 100–200 mm/year (polar desert) | Less than 50 mm/year (largest cold desert on Earth) |
| Human population | ~4 million (Inuit, Sámi and other indigenous peoples) | No permanent residents — 1,000–5,000 scientists at research stations |
| Governance | Divided between multiple nations (Canada, Russia, USA, Norway, Denmark/Greenland…) | Antarctic Treaty 1959 — international agreement; no country owns it |
| Characteristic animals | Polar bears, Arctic foxes, caribou, ringed seals, walrus | Emperor penguins, leopard seals, Weddell seals, albatross |
| Land vegetation | Tundra — mosses, lichens, sedges, dwarf shrubs | Almost none — only mosses and lichens on coastal rock outcrops |
The single most important contrast: Arctic = ocean surrounded by land. Antarctica = land surrounded by ocean. This explains most of the other differences.
Quick Check: State ONE key difference between the Arctic and Antarctica.
The Arctic is an ocean (the Arctic Ocean) surrounded by land, covered in floating sea ice typically 2–4 metres thick. Antarctica is a continent (a land mass) surrounded by the Southern Ocean, with an ice sheet up to 4.8 km thick resting on bedrock. Any one of the following also acceptable: Antarctica is colder (lowest −89.2°C vs −68°C); Antarctica has no permanent human residents (vs ~4 million in the Arctic); Antarctica is governed by international treaty (vs national ownership in the Arctic); Arctic has tundra vegetation on surrounding land (vs almost none in Antarctica).