PENN STATE (US) — Climate change induced warming affects ice and frozen ground at both the North and South poles, but the ramifications differ because of geography and geology.
“The polar regions, particularly the Arctic, are warming faster than the rest of the world,” says Michael Gooseff, associate professor of civil and environmental engineering at Penn State. “As a consequence, polar ecosystems respond directly to changes in the earth systems at the poles.”
Though different, the changes could be significant—not only on lcal environments but globally as well.
While the central part of the Arctic is composed of ice over water, northern Canada, Alaska, Siberia, and Greenland all have landmasses within the Arctic Circle. The associated land and water ecosystems are affected by melting ice and thawing soils, but in Antarctica, where much of the ice overlays a continent, the warming alters streams, lakes, and the tiny plants and animals that live there.
“Our focus on the north is in part because it is inhabited, but it is also because the ice there is more vulnerable,” Gooseff says. “Temperatures and snow and rain across the tundra shifts annually and seasonally. We know that fall is beginning later than it once did.”
In the Arctic, where there is more immediate feedback from the higher temperatures, the warming is degrading permafrost, the layer of the ground that usually remains frozen during annual thawing, resulting in a boggy, uneven landscape with a disturbed surface.
Subsequent rain or snowmelt erodes the surface carrying silt and sediment into bodies of water, changing the paths of rivers and streams. Debris flows are also a common ocurrence in degraded permafrost areas, Gooseff says. “Algae, insects and fish all must deal with this increased level of sediments.”
Extended frost-free time causes soils that do thaw annually to have longer active periods when microbes can mineralize nutrients. While the soils remain frost free longer, plants continue their normal cycle dictated by the length and intensity of daylight, which has not changed. Microbes may continue to create nutrients, but the plants no longer use them, so that when rain or meltwater comes the nutrients leach into the rivers and streams.
“That is exactly what we are seeing,” says Gooseff. “In September and October, we see a substantial increase in nutrients in the water. Concentrations increase many times for nutrients such as nitrate and ammonium.”
Another problem with degrading permafrost is the release of the carbon that had been permanently trapped in frozen organic materials in the frozen ground, because warming will eventually liberate carbon dioxide and methane into the atmosphere. “It is estimated that the permafrost contains twice the amount of carbon that is currently in our atmosphere,” Gooseff says.
Lakes and streams that exist in several polar desert oases, including the McMurdo Dry Valleys, are filled with a variety of life including microbial mats, plankton, and filamentous algae.
“While there are no bugs or fish in these waters, there are diverse microbial communities,” Gooseff says. “Some algae in the dry valleys go dormant for nine months or more and then begin to grow when hit by meltwater.”
Because there is so much permanent ice in Antarctica, the annual impact of increased temperatures on its environment is slower than in the Arctic. The huge expanse of white ice reflects some of the heat energy into the atmosphere. “We expect in the next several decades that we will see the Antarctic start to warm up,” Gooseff says.
The Antarctic permafrost is very dry with high nitrogen concentrations in some places. When water reaches some of these dry soils, it will mobilize the nutrients and increase potential habitat for freshwater aquatic communities in Antarctica. This climate change will alter the flow patterns, expand the stream networks, and change both the location of habitats and the timing of life cycles.
Understanding climate change in Antarctica has far-reaching implications.
“Understanding what happens in Antarctica is important to understand what happens on Mars,” says Gooseff. “There is potential for microbial communities on Mars, and if they exist they will probably be similar to the McMurdo Dry Valley communities.”
The National Science Foundation Office of Polar Programs supported this work.
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