Archived LIVE PolarConnect Event with Regina!
Regina held a live event on Tuesday 8 July 2014. You can access the video, slides, and audio in the PolarConnect Archives.
Tremendous stores of organic carbon frozen in permafrost soils have the potential to greatly increase the amount of carbon in the atmosphere. Permafrost soils may thaw sporadically and melting ground ice can cause land-surface sinking called "thermokarst failures". These failures change the rate and amount of carbon released with the unanticipated outcome being that soil carbon can be mixed-up from a depth and exposed to sunlight as the land surface is altered. Sunlight can photo-degrade or break-down organic carbon and alter the carbon's ability to support bacterial respiration to produce carbon dioxide. Whether sunlight and UV exposure will enhance or retard the conversion of newly exposed carbon to carbon dioxide is currently unknown—this study is providing the first evidence that this alteration will be amplified by photochemical processes and their effects on microbes.
The research team is trying to understand exactly how sunlight and bacteria degrade dissolved organic matter by determining how fast these processes convert newly released dissolved organic matter to carbon dioxide, compared to dissolved organic matter already in surface waters. The team is accomplishing their research objectives with a series of laboratory experiments to determine rates of photodegradation and microbial processing of dissolved organic matter from different sources, and a series of landscape comparisons and sampling transects to characterize dissolved organic matter degradation in small basins and large rivers extending from the headwaters to the Arctic Ocean. Ultimately, this research will attempt to answer questions such as whether carbon export from tundra to oceans will rise or fall and how reactive the exported carbon will be. The team hopes to be able to measure the ultimate impact of impending disturbances, including climate change, on the net carbon balance of the Arctic and its interaction with the global carbon cycle.
The research team was based out of Toolik Field Station, an 8-10 hour drive north from Fairbanks, Alaska. Toolik Field Station is operated by the Institute of Arctic Biology at the University of Alaska Fairbanks and has hosted hundreds of researchers and students every year since 1975. From the field station, the team traveled to their sites by foot, truck, boat and occasionally by helicopter.
Regina Brinker is a middle school science and engineering teacher in Livermore, California. She believes that it is her job to have students become so interested in science and technology that they want to continue studying these fields in high school and beyond. Mrs. Brinker engages students through hands-on inquiry and collaboration. Projects range from raising trout eggs, monitoring a pond's ecosystem, sending ping pong balls into space, and building robots and ROVs to international exchanges. Mrs. Brinker's students monitor seasonal changes of campus trees; this makes them better observers of the world around them. Development of this project inspired Mrs. Brinker to create a TED-Ed talk on phenology.
Through work with PolarTREC, Mrs. Brinker plans to give students a better understanding of the interrelationships of Earth's systems. Ecosystems don't exist in isolation. Mrs. Brinker wants her students to know how our collective actions influence climate change, both locally and around the Earth, and then choose to act responsibly.
Dr. Rose Cory works in the Arctic where climate warming is thawing frozen soil which may release tremendous stores of dissolved organic carbon to the Earth's surface. After having been trapped for millennia in the frozen soils this new carbon then becomes part of the modern carbon cycle. Dr. Cory finds that exposure to sunlight accelerates the return of this dissolved organic carbon to the atmosphere as carbon dioxide, which may further increase the rate of global warming. Because climate change is influencing our planet's evolution, understanding the fate of newly released carbon will help predict our future as a planet and society. Read more about Dr. Cory and her research here
George W. Kling is a professor in the Department of Ecology and Evolutionary Biology at the University of Michigan. He primarily studies aquatic ecology and biogeochemistry, and his research has focused on carbon and nutrient cycling, on using stable isotopes to understand trophic interactions, and on the integration of lakes and streams in a landscape context. His recent research has examined the role of microbial diversity in ecosystem function. He has worked internationally on arctic lakes and streams for approximately 25 years, and on tropical lakes in Africa.
Kling's scientific outreach to the public through interviews about his research on climate change and on the killer lakes of Cameroon includes articles in magazines and newspapers (e.g., National Geographic, Smithsonian), T.V. and radio broadcasts (e.g., CNN, BBC), and television films (e.g., BBC, Discovery). He has met regularly with U.S. Congress members to discuss issues of climate change and scientific integrity, and was lead author of the Union of Concerned Scientists – Ecological Society of America publication 'Confronting Climate Change in the Great Lakes Region' (2003). Kling is an associate editor for Limnology and Oceanography (2001-), an elected Fellow of the American Association for the Advancement of Science (1997-), and received a National Academy of Science Young Investigator Award (1993), a NSF Presidential Faculty Fellowship (1995), the United Nations Sasakawa Award (Certificate for Disaster Reduction, 2001), and the ASLO Ruth Patrick Award (2007).