This one hour webinar is a great look at the PolarTREC 2014-5 Antarctic expeditions. Each teacher presents on the research projects, implementation in the classroom, and outreach into communities.
Note: This event was not for our typical classroom-based education audience.
WAIS Divide (West Antarctic Ice Sheet), where the Velvet Ice team conducted its research, has recently be found to be one of the most vulnerable areas of Antarctica to global climate change. If recent predictions hold true, major glaciers in WAIS could collapse within 100 years, triggering massive shifts
This one hour event is an introduction to the expedition with Yamini Bala and her team. They address life at McMurdo and what it will be like at their remote field site at WAIS Divide (West Antarctic Ice Sheet).
PolarConnect event with Heidi Roop who is working with an Ice Core Drilling team on the West Antarctic Ice Sheet in Antarctica. A PDF of the slides is not available for this event.
This PolarConnect event was held on 16 December 2010 with Heidi Roop who is working with an ice core drilling team on the West Antarctic Ice Sheet. This live event was broadcast and had a live component at the AGU 2010 Fall Meeting.
Live from IPY! event with researcher Heidi Roop and other members of the ice coring team at WAIS Divide Camp, Antarctica. The presentation focused on project and the mechanics and science of ice coring.
Students will develop research questions that will help them develop an ecosystem profile (species/conditions etc.) of a local pond. Their results will be compared with data from the McMurdo Dry Valley Lakes in Antarctica. Discussions about climate and energy dynamics will be conducted as conclusions are drawn. A map and key for the local pond (species/locations/conditions) will be
During this lesson, students will learn basic glacial features and how to interpret Topographic maps and satellite images in order to create a model replica of a glacier valley. The Dry Valleys of Antarctica have classic glacial features, both in the barren valleys and in the remaining glaciers in the area. The glaciers are a major contributor to