The objectives of this lesson are:
* Students will know that climate change is happening most quickly in Arctic regions.
* Students will know that a warming climate is causing permafrost to thaw.
* Students will know that thawing permafrost is impacting infrastructure in Alaska, including roads and buildings.
* Students will design an engineering solution to create stable
In a “March Madness” game of survival of the fittest, will your microbe and its genes survive the test of changing conditions on Planet Earth and beyond? Students choose genes from a “toolbox” and pit their microbe against their classmates’, using critical thinking and argument writing to determine the microbe with the best chance of success. Based on PolarTREC
Students will use a model to explore the relationships between sunlight and release of carbon dioxide (CO2) from thawing Arctic watersheds.
After studying the carbon cycle, students are asked to reflect on how natural phenomena – thawing of permafrost, interactions of soil microbes on dissolved carbon, and amount of sunlight – interconnect and influence the release of CO2
Analogs are used in science investigations to better understand systems we can’t access ourselves. In this lesson, students explore the Dry Valleys of Antarctica to better understand microbial communities on early Earth and what might have been possible on ancient Mars. Students will examine photographs, written descriptions, and artistic renderings of early Earth, the Dry Valley lakes, and
On 6 October 2014, Capital Public Radio in Sacramento, CA interviewed Dawn Sumner, Tyler Mackey and Lucy Coleman on connections between the research in Lake Joyce, Antarctica, and work by the Mars Curiosity rover. To listen to the interview, click here.