Article in Polar Record written by ARCUS staff and PolarTREC alumni educators that shares impacts of participating in a Teacher Research Experience.
Abstract: PolarTREC-Teachers and Researchers Exploring and Collaborating (PolarTREC) has provided the opportunity for over 160 K-12 teachers and informal science educators from the USA to work directly with scientists in the Arctic and the Antarctic. As a Teacher
This resource is a 2-minute immersive video that takes students inside the Permafrost Research Tunnel outside of Fairbanks, Alaska. It includes footage of both the new and old sections of the tunnel.
Objectives
Through watching this video, students will get to see what permafrost looks like from the inside, identifying typical features geological features (ex. ice wedges). Through the
This lesson plan transports students to two field sites outside of Fairbanks, Alaska to investigate the interconnected relationships between climate change and permafrost. Students will use authentic field data from site photographs, soil temperature, and thaw depth measurements to draw inferences. An ESRI StoryMap, faux field journal, and 360 site images are used to engage students in the inquiry
This mini exhibit explores the science behind climate change and introduces current climate change research to the public. Panels cover the topics of changing climate, ocean acidification and sea level rise, giving examples of how data is collected and current research in these fields. The exhibit also provides websites for further exploring climate change impacts.
This one hour webinar is hosted by Dominique Richardson and the team studying the Antarctic Ice Stream Dynamics was a special event to celebrate Earth Day 2015.
The long-term objective of PolarTREC teacher Lesley Urasky's expedition research in Antarctica (Glacial History in Antarctica) is to determine the rate at which glaciers have receded since the Last Glacial Maximum. This lesson is designed to give students an understanding of the Last Glacial Maximum, the climatic conditions that lead to glacial periods, and how the rate of glacial