Glaciers and climate change

Glacial ice can range in age from several hundred to several hundreds of thousands years, making it valuable for climate research. To see a long-term climate record, scientists can drill and extract ice cores from glaciers and ice sheets. Ice cores have been taken from around the world, including Peru, Canada, Greenland, Antarctica, Europe, and Asia. These cores are continuous records providing scientists with year-by-year information about past climate. Scientists analyze various components of cores, particularly trapped air bubbles, which reveal past atmospheric composition, temperature variations, and types of vegetation. Glaciers preserve bits of atmosphere from thousands of years ago in these tiny air bubbles, or, deeper within the core, trapped within the ice itself. This is one way scientists know that there have been several Ice Ages. Past eras can be reconstructed, showing how and why climate changed, and how it might change in the future.

Gangotri GlacierThis false-color satellite image shows the Gangotri Glacier, situated in the Uttarkashi District of Garhwal Himalaya. Currently 30.2 kilometers (19 miles) long and between 0.5 and 2.5 kilometers (0.31 to 1.5 miles) wide, Gangotri glacier is one of the largest in the Himalaya. Gangotri has been receding since 1780, although studies show its retreat quickened after 1971. Note that the blue contour lines drawn here to show the recession of the glacier's terminus over time are approximate. Over the last 25 years, Gangotri glacier has retreated more than 850 meters (930 yards), with a recession of 76 meters (83 yards) from 1996 to 1999 alone. —Credit: NASA, based on data provided by the ASTER Science Team. Glacier retreat boundaries courtesy the Land Processes Distributed Active Archive Center.

Scientists are also finding that glaciers reveal clues about global warming. How much does our atmosphere naturally warm up between Ice Ages? How does human activity affect climate? Because glaciers are so sensitive to temperature fluctuations accompanying climate change, direct glacier observation may help answer these questions. Since the early twentieth century, with few exceptions, glaciers around the world have been retreating at unprecedented rates. Some scientists attribute this massive glacial retreat to the Industrial Revolution, which began around 1760. In fact, several ice caps, glaciers and ice shelves have disappeared altogether in this century. Many more are retreating so rapidly that they may vanish within a matter of decades.

Scientists are discovering that production of electricity using coal and petroleum, and other uses of fossil fuels in transportation and industry, affects our environment in ways we did not understand before. Within the past 200 years or so, human activity has increased the amount of carbon dioxide in the atmosphere by 40 percent, and other gases, such as methane (natural gas) by a factor of 2 to 3 or more. These gases absorb heat being radiated from the surface of the earth, and by absorbing this heat the atmosphere slowly warms up. Heat-trapping gases, sometimes called “greenhouse gases,” are the cause of most of the climate warming and glacier retreat in the past 50 years. However, related causes, such as increased dust and soot from grazing, farming, and burning of fossil fuels and forests, are also causing glacier retreat. In fact, it is likely that the earliest parts of the recent glacier retreats in Europe were caused by soot from coal burning in the late 1800s.

As dramatic as the retreat of one glacier may be, scientists learn the most about global climate by studying many glaciers. The World Glacier Monitoring Service (WGMS) tracks changes in more than 100 alpine glaciers worldwide. Forty-two of those glaciers qualify as climate reference glaciers because their records span more than 30 years.

The WGMS reports glacier mass balance changes in millimeters of water equivalence. (There are 25.4 millimeters in an inch.) If all the lost or gained glacial ice were converted to water and spread evenly over glacier surface area, the depth of that water layer is the water equivalence. In State of the Climate in 2018, the American Meteorological Society reported that mean annual glacier mass balance was -921 millimeters for the 42 reference glaciers, and -951 millimeters for all glaciers monitored in 2017.

WGMS graphThis graph shows mass balance of the WGMS 37 reference glaciers each year since 1968 (red bars), along with the total mass loss over time (black line).. —Credit: State of the Climate in 2018. Bull. Amer. Meteor. Soc

Last updated: 16 March 2020