Greenland’s Tracy and Heilprin Glaciers Melt

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The climate is changing. Retreating glaciers; rising sea levels; hotter and more acidic oceans; and more frequent, stronger storms: all of these changes can be traced to an increase in the earth’s average temperature, which is about 2°F higher today than it was near the turn of the twentieth century.

But the consequences of climate change are more complicated and connected than a simple list of weather events implies. For example, floods caused by rising sea levels can destroy infrastructure and displace communities, exacerbating issues like poverty, instability, and migration. 

Enter Greenland, where a changing ecosystem illustrates the complexity of this issue. 

For at least five thousand years, sea levels were  more or less stable. But since the end of the nineteenth century, average sea level has risen about eight inches, and it is rising faster now: roughly one-third of that increase has happened in the past twenty-five years. 

So why are sea levels rising? A major factor is glacier melt, and scientists are particularly concerned about Greenland’s melting. Eighty percent of Greenland is covered by an ice sheet, or large area of land covered in glacial ice. It’s one of only two in the world. (The other is Antarctica.)

Melting is not normally cause for alarm. It is a seasonal process: ice sheets melt in the summer, and then typically regain their mass through water that refreezes in the winter. 

Here is how the process of melting and refreezing has looked for thousands of years:

But climate change has interrupted this process. Exposed to warmer weather for a longer portion of the year, Greenland is now experiencing a longer melt season than normal, which means it is shrinking. Think of it as a receding hairline: hair still grows, but not quickly enough to outpace hair loss.

“Feedback loops”: Longer melting periods causes more ice to melt even faster.

Most scientists agree that feedback loops—or self-reinforcing cycles—are occurring in Greenland. This means that as hotter temperatures spur more melting and longer melt seasons, two related consequences occur: First, older, darker ice is exposed. Like a black shirt absorbing more heat than a light-colored one, this darker ice absorbs more of the sun’s energy and accelerates the natural melting cycle. Second, meltwater also travels down moulins, or ice tunnels, that extend to the bottom of the ice sheet, and lubricates the space between the ice and the bedrock. This causes ice to break off and move more quickly out to sea where it will melt. So, again, the more ice that melts on the surface, the more quickly glacier melt occurs.

Not only is melt season now a couple of months longer, but more of the ice sheet is melting.  The island lost around four trillion tons of ice between 1992 and 2018, according to one study.

The video below illustrates this phenomenon. In the map on the left, you can see the area where melting was observed expand every year. In the graph on the right, you can see the amount of ice rise each winter and fall each summer. But every year, more is lost than gained.

And as more ice melts, the higher sea levels rise.

Global Warming and Rising Sea Levels

Rising sea levels have their own adverse effects. 

Higher sea levels threaten coastal cities, increase flooding, and intensify storms. This puts millions of people at risk: 40 percent of the U.S. population lives in coastal areas, and eight of the world’s ten largest cities are near a coast.

This map shows coastal urban areas, and the percentages of their populations that would be affected by rising sea levels if global temperatures rose to 4°C higher than they were before the Industrial Revolution. If the climate keeps getting warmer and ice in Greenland and elsewhere continues to melt at a fast pace, many of these cities could be in danger.  

Rising Sea Levels

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If all of Greenland’s ice melts—which could happen if temperatures rise by more than 2°C—sea levels will rise by twenty-three feet. That is higher than the average two-story house. That is why scientists are tracking Greenland’s ice loss so carefully.

There is no going back for Greenland. The feedback loops created by rising temperatures mean that Greenland will probably continue to rapidly lose ice for years to come, even if greenhouse gas emissions completely stop tomorrow. But scientists believe that by studying Greenland, they can achieve a better understanding of the wide range of consequences climate change will have on other parts of the world—and help people prepare to adapt to the new reality it will bring. 

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