Tropical glaciers are melting fast: Looking for clues to climate change

Tropical glaciers are melting fast: Looking for clues to climate change

Madhurita Goswami, Dec. 18, 2019

Most of us associate glaciers with Antarctica or the northern ice-sheets of the Arctic and Greenland. It may come as a surprise that scientists Alice M. Doughty and Meredith Kelly are studying tropical glaciers at the Rwenzori Mountains of Uganda to improve our understanding of climate change.

The Rwenzori lies only 23 minutes north of the Equator and almost 30 degrees east of the Prime Meridian. There are glaciers here because the life cycle of tropical glaciers isn’t about location but height. Reaching Rwenzori’s glaciers means climbing at least 4,000 meters (more than 13,000 feet) above sea level just to get to the foot of them. Still, in a warming world, height can’t protect these once mammoth ice formations as they rapidly retreat.

Even for Kelly, the term glacier raises images of classic ice masses in the Swiss Alps, which partially melt during the summer and then grow again in the winter due to snowfall.

Meredith Kelly leads expeditions to sample moraines at the Rwenzori glaciers. (Abigail Foerstner)

“Tropical glaciers are really different because summer and winter temperatures are almost the same,” said Kelly, an associate professor of Earth Science at Dartmouth College.

Studies on tropical glaciers have confirmed that they reached their maximum extent around the same time that high-latitude glaciers were at their maximum during the last great ice age some 18,000 years ago. This tells scientists that there was a synchronized warming at the end of the last ice age.

“Tropics are located far from mechanisms of climate change such as summer insolation [exposure to the sun] in northern high latitudes or direct effect of ice-sheets. So, they might be responding to CO2 (carbon dioxide) or other mechanisms we haven’t defined yet,” Kelly said at the 2019 Comer Climate Conference held in southwestern Wisconsin in early October.

CO2 is a greenhouse gas is warming the Earth as it collects in the atmosphere at ever higher levels due to emissions from human use of fossil fuels that include coal, gasoline and natural gas.

Alice Doughty works on glacial models based on data obtained from the Rwenzori glaciers. (Abigail Foerstner)

Kelly proposed that the temperature gradient between the poles and the tropics might have played a role. When the gradient is smaller, there is less outflow of heat from the tropics.

For a long time, scientists puzzled over factors driving changes in tropical glaciers. Initially, they attributed the main cause to precipitation as seasons in the tropics can be divided into wet and dry.

However, “tropical glaciers couldn’t have advanced (during the last glacial maximum) due to precipitation alone. There had to have been substantial cooling at high altitudes,” said Doughty, a visiting assistant professor of geology at Bates College. “We don’t have strong thermal seasons in the tropics. So, these glaciers were/are responding to what’s happening in the tropical atmosphere.”

A vast number of tropical glaciers are in the Andes in South America. Others are on Mt. Kenya in Kenya, Mt. Kilimanjaro in Tanzania and the Rwenzori Mountains in Uganda and the Democratic Republic of Congo. Some are located in Papua, New Guinea.

“It takes a village” – How locals are helping researchers in Uganda

Researchers studying tropical glaciers, which are relatively small, face some unique challenges. Not the least of them is having to hike up mountains with their equipment for days on end. They can’t reach the sites by helicopters or cars. Local guides, who know the mountain trails, become essential to their success.

Moraines (ridges of boulders) left behind by retreating glaciers are used to determine their past extents. However, looking for boulders in the Rwenzori Mountains is like playing a game of hide and seek, said Doughty, who works on glacial modeling. As many as 58 people have to work on finding these boulders in the woods. “It takes a village,” said Doughty.

“It is difficult to find these boulders as they are covered with vegetation, which can be up to a meter thick,” said Kelly, who samples the moraine boulders. In this case, too, locals help to cut down the overgrowth with their machetes.

The mat of vegetation conceals massive gaps between boulders, Doughty said and hinted at the risk of accidents. But walking is the only way to find boulders, which can’t be spotted from space or with drones.

Tropical glaciers on the peaks of the Rwenzori Mountians in Uganda are small and rapidly receding (Meredith Kelly/Alice Doughty)

Doughty, at first, was uncomfortable with the idea of guides and porters, and the dynamics of teaming everyone together. “So, we talked about jobs in the area. In mountain communities, being a porter is a huge part of that and some were raising money to go to college. I realized we were supporting the economy,” she said.

Rwenzori is also the name of a national park managed by a government agency, the Uganda Wildlife Authority, and it also runs the porter service. “We have really benefited from its system, which allows us to find collaborators in Uganda,” Kelly said.

Photo at top: Local guides play an important role in finding boulders left behind by retreating glaciers. (Meredith Kelly)

Glaciers as “global thermometers” show the fast pace of melting in a warming world

Glaciers as “global thermometers” show the fast pace of melting in a warming world

Madhurita Goswami, Dec. 18, 2019

Glaciers across the globe behave in a synchronized manner, said geologist Thomas Lowell at the recent Comer Climate Conference, an annual national conference held in southwestern Wisconsin. Not only does he study glaciers around the world to reach this conclusion but also compared data obtained by separate dating techniques.

Sounding the alarm, as we warm temperatures the glaciers retreat faster, he said. This, in turn, would change the sea levels in coming years by a greater extent than people imagine now, Lowell added.

The results show that incoming solar radiation, which varies seasonally in the two hemispheres, is not the major factor affecting climate change and has implications for identifying other factors.

“I have looked at glaciers from central-northern Greenland to Antarctica,” said Lowell, a professor of geology at the University of Cincinnati. “They were universally behaving in the same way during the last glacial maximum. They were out, bounced around a little bit and receded at the same time.”

The maximum reach of the ice age, or glacial maximum, left its mark on the Earth’s landforms some 18,000 years ago.

Thomas Lowell gives his presentation on comparing data from glaciers around the world (Abigail Foerstner)

Glaciers are “global thermometers” which track temperatures and can be used for reconstruction of our past climate. However, they don’t leave a continuous record. “We get different pieces from different places and try to match them. They might not match because there are some missing pieces,” Lowell said. There is, however, substantial correlation in the data that he is trying to quantify.

The pattern of glacial movement also shows how sensitive they are. Lowell said, “The zigs are around a thousand years apart. It shows, in my opinion, that a temperature pattern was superimposed on the glaciers. It was generally cold but there were warmer and colder times.”

Of the two techniques used to obtain glacial data, radiocarbon dating is the traditional one. It requires accumulation of organic material around the periphery of a retreating glacier. Scientists study the decay of carbon-14 in this organic matter. The other dating technique relies on moraines, a chain of boulders tossed behind by retreating glaciers.

When particles produced by galactic cosmic rays strike the rock surface, beryllium-10, a radioactive isotope of beryllium, is produced. Scientists can analyze beryllium-10 decay to find out when it was generated, which corresponds with moraines losing their ice cover.

“Each technique has its advantages and limitations. Lowell’s emphasis on observing both the chronologies and finding a correlation between them is a more compelling reconstruction of what happened in the past,” said Jerry McManus, a climate scientist and professor at the Lamont-Doherty Earth Observatory of Columbia University.

“In cases where organic matter is available, it is relatively easier to take measurements and more data can be quickly produced. However, the amount of carbon-14 in the earth’s atmosphere changes over time and it is a bit of a moving target,” he said. On the other hand, many glacial sites don’t have moraines and so beryllium-10 dating is not an option there.

Photo at top: Huge icebergs are breaking off the Greenland glaciers. (Gary Comer/Comer Family Foundation)


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