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
NASA’s Operation IceBridge uses remote sensing techniques to build a picture of parts of our world not accessible or easily observed by humans. Flying 1500 feet above sea and land ice, the science team uses LiDAR, Radar, Infrared imaging, and high resolution digital imagery to collect information about our polar regions year after year. In this classroom project, inspired and
Interview with PolarTREC teacher Paula Dell and her students from Lindblom Math & Science Academy about their underwater camera probe called "Fish Spy 2" to study icefish in Antarctica.
Article featuring PolarTREC teacher Paula Dell (Biology of Antarctic Fishes 2011, 2013) and her students from Lindblom Math & Science Academy high school in Chicago, Illinois who have created a Fish Spy robotic camera to study icefish in Antarctica.
NASA’s Operation IceBridge, the largest airborne survey of Earth’s polar ice, uses remote sensing techniques like LiDAR (light detection and ranging), snow- and ice-penetrating radar, high resolution digital imaging, and infrared cameras to collect information on our changing ice sheets and sea ice. Several times each year a science team and flight crew head out on month-long campaigns in
The PolarTREC program and my experience with NASA’s Operation IceBridge during the 2016 Spring Arctic Campaign in Greenland has reinforced my belief in teacher-researcher collaborations as a powerful tool for engaging students in STEM and giving them the chance to think and explore career possibilities outside of the four walls of their classrooms. One of the most effective
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