New Arctic Coastlines Are Emerging as Glaciers Melt — What That Means for Our Planet

Geodiversity of new coastlines developed after retreat of Arctic marine-terminating glaciers.

Geodiversity of new coastlines developed after retreat of Arctic marine-terminating glaciers. a, Young delta system accumulated in the lagoon exposed by Recherchebreen, Svalbard. b, Rocky cliffs and morainic cliffs released from retreating Samarinbreen, Svalbard. c, Juvenile beach system in Brepollen supplied by glacial sediment dropping from remnants of ice cliffs. d, Erosion of a lateral moraine by calving waves from Eqip Sermia, Western Greenland, leading to extension of the spit system along the southern coast. Credit: b,c, Aleksandra Osika. Nature Climate Change (Nat. Clim. Chang.) ISSN 1758-6798 (online)


A Changing Arctic

Over 2,400 kilometers of new Arctic coastline have appeared in just 20 years.

That’s like adding a whole new stretch of shore equal to the length of the U.S. West Coast — all because of melting glaciers. As temperatures rise across the globe, nowhere is changing faster than the Arctic. In fact, the Arctic has warmed nearly four times faster than the rest of the planet in the past few decades.

And with that warming comes dramatic change: the disappearance of ice, the reshaping of coastlines, and the emergence of land that hasn’t seen the light of day for thousands of years.

Why Glaciers Matter

Let’s start with the basics. Some glaciers, called marine-terminating glaciers, end in the ocean instead of on land. These icy giants slowly move downhill and, when they meet the sea, they break off chunks of ice into the water — a process known as calving.

But as the planet gets warmer, these glaciers are shrinking. Warmer air and ocean water are causing them to melt and pull back from the coast. When they do, they uncover land that used to be buried under thick ice.

This retreat is happening all over the Northern Hemisphere — from Alaska to Greenland — and it’s changing what our maps look like.

What Happens When Glaciers Retreat?

When a glacier melts and retreats, it exposes new ground beneath it. That newly uncovered area often becomes coastline, especially when the glacier used to flow into the ocean.

These brand-new coastal areas are made of soft sediments like sand and gravel, or sometimes smooth, polished rock. Because this land has been hidden under ice for so long, it hasn’t had time to settle or stabilize. That means it can be quickly reshaped by wind, waves, and weather.

Scientists call these places “paraglacial coasts” — a term that simply means land newly exposed by melting glaciers. These coasts are among the most dynamic and fast-changing landscapes in the world.

Where Is This Happening?

Between 2000 and 2020, researchers tracked over 2,466 kilometers of new coastline created by glacier retreat.

Here’s where the biggest changes are:

  • Greenland: 66% of the new coastline came from here — over 1,600 km.

  • Northern Canada, Russia, and Svalbard: Each contributed around 9–10% of the new coastlines.

  • Alaska and Southern Arctic Canada: Though smaller in size, these areas had some of the most efficient coastline formation per glacier.

This isn’t just about flat beaches — new islands are also appearing. In fact, 35 new Arctic islands were identified between 2000 and 2020, most of them in Greenland.

Why This Matters to People and Nature

New coastlines might sound exciting — and they are — but they come with both risks and opportunities.

Risks

  • Tsunamis and landslides: Some new coasts are unstable and prone to large waves caused by landslides, falling icebergs, or glacier collapse. A tragic example happened in Greenland in 2017, when a tsunami destroyed homes and took lives.

  • Tourism safety: Melting glaciers change the landscape rapidly, affecting local communities and visitors who camp or sail near them.

Opportunities

  • New habitats: As glaciers melt, they make room for new ecosystems. Plants, animals, and even fish begin to move in and adapt to these fresh environments.

  • Natural resources: Some of the newly exposed land is rich in materials like sand and gravel, which could be valuable for local economies, especially in Greenland.

What’s Next?

Glaciers are expected to keep retreating as global temperatures rise. That means even more coastlines and islands will appear in the coming decades. But this change isn’t always predictable. Some glaciers move slowly, while others retreat in big bursts. And the way the land responds depends on things like the type of rock, the presence of permafrost (permanently frozen ground), and the local climate.

Scientists emphasize the importance of monitoring these new areas closely. Understanding how they’re forming — and how fast — helps us prepare for what’s ahead, from rising sea levels to new environmental challenges.

What You Can Do

Even if you’re far from the Arctic, there are still ways you can make a difference.

  • Read and share reliable information about changes happening in the Arctic and around the world.

  • Organizations and scientists are doing amazing work using satellite data and field studies. Supporting or sharing their findings helps spread awareness.

  • Advocate for climate action, including clean energy and reduced carbon emissions, to help slow ocean warming.

  • Vote for leaders and policies that take action on climate change.

  • Hold your local, state, and national elected officials accountable for taking climate action and protecting our water, air, and health.

Closing Thought

The Arctic is not a frozen, unchanging place — it’s alive, moving, and reacting to what we do. The more we understand these changes, the better we can care for our planet.


Source: Kavan, J., Szczypińska, M., Kochtitzky, W., Farquharson, L., Bendixen, M., & Strzelecki, M. C. (2025). New coasts emerging from the retreat of Northern Hemisphere marine-terminating glaciers in the twenty-first century. Nature Climate Change. https://www.nature.com/articles/s41558-025-02282-5?error=cookies_not_supported&code=7999c3fc-517f-4c3a-8202-1dd867b0ff9d.

Global Impact of Melting Snow and Ice

Two Antartica icebergs floating on calm water with intricate, wave-like formations, set against a dark icy landscape in a serene polar environment. Photo by Torsten Dederichs on Unsplash.
Two Antartica icebergs floating on calm water with intricate, wave-like formations, set against a dark icy landscape in a serene polar environment. Photo by Torsten Dederichs on Unsplash.

How Melting Ice Shapes Our Climate, Water, and Future—and What We Can Do to Protect It

Did you know that Greenland is losing 30 million tons of ice every hour? This isn’t just a shocking statistic—it’s a wake-up call. The melting of the world’s ice isn’t just a problem for cold regions; it’s an issue that impacts all of us, from the water we drink to the air we breathe. This week we examine the importance of Earth’s ice, the alarming changes it’s undergoing, and why it matters to your life.

The Big Picture: What Is the Cryosphere?

The “Cryosphere” might sound like a complicated word, but it simply means all the parts of Earth covered in snow and ice. This includes glaciers, ice sheets, permafrost (frozen ground), and sea ice.

Why does the cryosphere matter?

  • Temperature Regulation: The cryosphere reflects sunlight, keeping the planet cool, much like a natural air conditioner.

  • Water Storage: It stores about 70% of the world’s fresh water, feeding rivers and supporting billions of people.

Without the Cryosphere, Earth would be hotter, drier, and much less hospitable.

Alarming Changes in Ice and Snow

The Cryosphere is changing fast, and the consequences are already being felt worldwide. Greenland is losing ice at an unprecedented rate, enough to raise sea levels significantly in the coming decades. Glaciers in the Alps and Himalayas are melting at record levels, threatening water supplies for millions of people downstream.

In addition, Antarctic sea ice is shrinking, with three consecutive years of record lows. This destabilizes the Antarctic ice sheet, which could lead to catastrophic sea-level rise. And, frozen ground in Arctic regions is thawing, releasing harmful greenhouse gases like carbon dioxide and methane. This accelerates global warming and damages infrastructure in those regions.

Why It Matters to You

Melting ice may seem like a distant problem, but its effects are closer to home than you think.

  • Rising Seas: As ice melts, sea levels rise, threatening coastal cities and communities. Major cities like New York, Miami, and Mumbai face increased flooding risks.

  • Water Supply: Snow and ice act as reservoirs, releasing water during warmer months. With less snowpack, regions like the Himalayas and Andes face water shortages, impacting agriculture and drinking supplies for billions.

  • Changing Weather: Melting ice disrupts weather patterns, leading to stronger storms, unpredictable rainfall, and even impacts on fisheries as oceans warm and acidify.

The Path Ahead: What Scientists Say

The Cost of Inaction

If emissions continue at current levels, global temperatures could rise by 3°C or more by the end of this century. This would push many regions beyond their ability to adapt, leading to economic and human costs that are unimaginable.

Hope Through Action

The good news? Scientists agree that if we act now to limit warming to 1.5°C, we can slow ice loss and reduce long-term damage. This requires cutting emissions by 50% by 2030 and reaching net-zero by 2050.

What Can Be Done?

Global Solutions

To address the challenges posed by melting ice and its global impacts, reducing emissions is a critical step. Transitioning to renewable energy sources like wind and solar can significantly cut greenhouse gas emissions, slowing the pace of global warming and ice loss. Additionally, protecting vulnerable areas is essential. Investing in resilient infrastructure and implementing policies designed to safeguard communities can help mitigate the risks of rising seas and water shortages, ensuring these regions are better prepared for the future.

Individual Steps

You don’t have to be a scientist or policymaker to make a difference. Here’s how you can help:

  • Advocate for climate-friendly policies in your community.

  • Use public transport, conserve energy, and support sustainable products.

  • Spread awareness by sharing what you’ve learned with friends and family.

Summing Up

Saving the world’s ice isn’t just about preserving glaciers—it’s about protecting our homes, food, and future. The actions we take today will shape the world for ourselves as well as future generations. Each degree of warming we prevent reduces the risks to our planet and ourselves. Let’s work together to ensure that ice continues to cool the Earth, sustain life, and inspire hope for a better tomorrow.


International Cryosphere Climate Initiative. (2024). State of the cryosphere 2024: Lost ice, global damage. International Cryosphere Climate Initiative. Retrieved from https://iccinet.org/statecryo24/.

New Study Shows West Antarctic Ice Sheet Might Be Safer from Collapse This Century

Lemaire Canal in West Antarctic
Glacier breaking edge in the Lemaire Canal. The Lemaire Canal is a narrow ship passage. It separates the island of Booth from the Antarctic Peninsula. Credit: W. Bulach, CC BY-SA 4.0, via Wikimedia Commons, December 8, 2005.

Some Climate Threats May Be Less Urgent, But Action Is Still Needed to Protect Ice Sheets

A recent study led by researchers at Dartmouth College brings some good news about the West Antarctic Ice Sheet, particularly Thwaites Glacier. Scientists have found that this massive ice sheet might be less likely to collapse during the 21st century than we previously feared. This discovery could mean that the threat of rapidly rising sea levels is not as immediate as some had thought.

What Is MICI and Why Does It Matter?

MICI stands for Marine Ice Cliff Instability. It’s a big concern in the world of climate science. The idea is that if the floating ice shelves around Antarctica collapse, they could expose tall ice cliffs. These cliffs might break apart quickly, leading to more ice melting and causing sea levels to rise around the world. Previous studies suggested that MICI could cause the West Antarctic Ice Sheet to collapse, leading to significant sea level rise by the end of this century.

How This Study Was Done

Scientists from several universities used advanced computer models to simulate what might happen to Thwaites Glacier if its ice shelf collapses. They applied new methods to gain a clearer understanding of the ice sheet’s stability. These models are more detailed and realistic than the ones used in older studies.

The new methods took into account how the ice both bends and breaks. This made the models more realistic in showing how the ice sheet might behave if the ice shelves collapse and tall cliffs are exposed.

The study also used more advanced and detailed models. By using three different models (ISSM, STREAMICE, and Úa), the researchers made sure their results were not limited to just one type of model. This approach gave a clearer picture of how stable the West Antarctic Ice Sheet might be, especially concerning MICI.

Key Findings: Less Risk of Collapse

The study’s results are reassuring. Even in the worst-case scenarios, where the ice shelf collapses completely, the models show that the glacier would likely remain stable throughout the 21st century. The exposed ice cliffs wouldn’t be tall enough to cause the runaway collapse that was previously feared.

Two important factors help keep the glacier stable:

  1. Faster Ice Movement: If the ice shelf collapses, the ice behind it would begin moving faster, which surprisingly helps prevent the cliffs from breaking apart.

  2. Thinning Ice: The ice near the front would become thinner, making the cliffs less likely to reach dangerous heights.

Why This Matters for Sea Levels

This study suggests that the scenarios where sea levels rise quickly due to the collapse of the West Antarctic Ice Sheet might not happen as soon as we thought. However, the scientists warn that other processes could still cause the ice to melt over the long term. We shouldn’t assume everything is fine, but it’s a relief to know that we might have more time to address these challenges.

Call to Action

This study is a reminder that while some climate threats may be less urgent than we feared, we still need to take action. Ice sheets like the West Antarctic are still at risk in the long run.


Morlighem, M., Goldberg, D., Barnes, J. M., Bassis, J. N., Benn, D. I., Crawford, A. J., Gudmundsson, G. H., & Seroussi, H. (2024). The West Antarctic Ice Sheet may not be vulnerable to marine ice cliff instability during the 21st century. Science Advances, 10(eado7794).