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What is Permafrost?

Visual representation of permafrost layers
Illustration showing permafrost layers below the surface

Permafrost is ground that stays completely frozen for at least two years in a row. It's not just frozen soil - it can be soil, rock, or sediment that contains ice and organic material. The name comes from "permanent frost" because it stays frozen year-round.

Permafrost is different from regular frozen ground because it doesn't thaw in the summer. Instead, only the top layer (called the active layer) thaws and refreezes each year. Below that active layer, the ground stays frozen solid.

Where is Permafrost Found?

World map showing permafrost distribution
Map showing global permafrost distribution

Permafrost covers about 25% of the land in the Northern Hemisphere. Most of it is found in:

1

Arctic Regions

Alaska, Northern Canada, Greenland, Siberia

2

High Mountains

Rocky Mountains, Alps, Himalayas

3

Antarctica

Frozen ground beneath the ice

Permafrost forms where the average air temperature is below freezing (0°C or 32°F). The thickness varies from just a few feet to over 4,900 feet (1,500 meters) deep in parts of Siberia!

The surface above permafrost is often covered by a unique ecosystem called tundra - a cold, treeless landscape with special plants and animals adapted to the harsh conditions.

Why Permafrost Matters

Illustration showing carbon storage
Carbon stored in permafrost over thousands of years

Permafrost is like a giant freezer preserving ancient plants and animals. Over thousands of years, dead plants didn't fully decompose because of the cold. Instead, they turned into organic carbon stored in the frozen ground.

Scientists estimate that permafrost contains about 1,500 billion tons of carbon - that's almost twice as much carbon as is currently in the atmosphere! This makes permafrost incredibly important for Earth's climate.

Carbon Storage

Holds vast amounts of ancient plant carbon

Water Regulation

Controls water flow in Arctic ecosystems

Land Stability

Provides foundation for buildings and roads

Permafrost also supports unique ecosystems and helps regulate water flow in northern regions. Indigenous communities have lived on permafrost for thousands of years, building their homes and ways of life around these frozen landscapes.

Thawing Permafrost

Illustration showing effects of thawing permafrost
Effects of thawing permafrost on landscapes

As Earth's climate warms, permafrost is thawing at an accelerating rate. This thawing causes significant changes:

1

Land Changes

Ground sinks, causing "drunken forests" and damaged buildings

2

Carbon Release

Thawed organic matter decomposes, releasing CO₂ and methane

3

Methane Emissions

Bubbles of methane rise from thawing lakes

When permafrost thaws, microbes begin decomposing the ancient organic material, releasing carbon dioxide and methane (a powerful greenhouse gas) into the atmosphere. This creates a dangerous cycle: warming causes thawing, which releases gases that cause more warming.

Scientists are concerned because methane emissions from thawing permafrost could significantly accelerate climate change. The changes in soil moisture and landscape also affect Arctic plants and animals.

Permafrost Quiz

Test your permafrost knowledge with this quiz! Answer all 5 questions to see how much you've learned.

1. What is the definition of permafrost?
2. What percentage of the Northern Hemisphere's land is covered by permafrost?
3. What important material is stored in permafrost?
4. What greenhouse gas is released when permafrost thaws?
5. What is the name of the top layer that thaws each summer?

Frequently Asked Questions

Here are answers to some common questions about permafrost:

Amazing Permafrost Facts

Discover some fascinating information about Earth's frozen ground:

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