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
Through activities, video observation, experimentation and the construction of a Remotely Operated Vehicle (ROV) students will learn about the chemical and physical properties of sea ice.
Objectives
Students will be able to answer main questions of where sea ice is, how it is formed, why the ice is important, how it is classified by indigenous people and scientists, how
Article from The Shorthorn - University of Texas at Arlington's student newspaper detailing PI Laura Gough's participation in a PolarTREC Live from IPY! Event. Laura is working with PolarTREC teacher Cathy Campbell at Toolik Station, Alaska this summer.
This website provides information on the Arctic ground squirrel including facts and pictures explaining the adaptations the squirrel has to survive the harsh Arctic winters.
Maggie Prevanas joined scientists in the Bering Sea where sampling to measure the productivity of the Bering Sea Ecosystem was conducted. Maggie learned about the role microscopic organisms, diatoms, play in algae blooms, carbon cycling, and global warming. Maggie developed a lesson using scientific illustration to introduce diatoms to her students.
A great resource that includes content and lessons for all grades. You can sign up to receive seeds that have either been in space or on Devon Island plus seeds that have not been exposed to harsh conditions. Students will be able to participate in a blind study to see if they can determine which seeds are the harsh environment
WHOI is the world's largest private, nonprofit ocean research, engineering and education organization. This site has information on oceans from climate to ocean life to ships and technology.