This lesson focuses on the diffusion of gas molecules across the cuticle membrane of sea spider legs and the role body size plays in the ability of sea spiders to uptake gases. Students construct model sea spider legs of varying diameters and use them to investigate the relationship between surface area-to-volume ratios and diffusion.
Ice that forms in the polar oceans is an important driver behind the global climate. This ice is physically different from frozen precipitation in a number of different ways. In this brief inquiry activity, students make qualitative observations about two types of ice cubes and deduce ice composition based on their observations. This activity may serve as an introduction to
This 1 hour webinar celebrates Antarctica Day 2015 with PolarTREC teacher Michelle Brown and the Human Impacts in Antarctica 2015 expedition. Michelle and her team are on the ice, at McMurdo Station, sharing their research project with the webinar audience.
This one hour webinar features Alex Eilers and the team studying Weddell Seals in the Ross Sea. The team shares their research with the audience and honors the importance of Antarctica Day. The event celebrates the international treaty stating that Antarctica is set aside for peaceful scientific purposes.
This is a one hour webinar hosted by PolarTREC teacher Andre Wille at Toolik Field Station, Alaska. The work presented is part of the Arctic Ground Squirrel Study 2014.
This PowerPoint presentation could be used as part of an introductory or supplementary unit on Antarctica. The presentation includes stunning visuals and general facts about Antarctica.
Jeanine Gelhaus <gelhaje [at] medford.k12.wi.us> Capstone Project Fall 2013. Integrated Life and Earth Sciences in the Polar Regions.
Through investigation, you will determine which solution has the highest density.
Objective
To determine, through experimentation, which of a variety of solutions has the highest density.
Preparation
Background: The waters of the ocean are constantly moving in many different ways. The surface of the ocean rises and falls in rhythm. These movements, in the form of