How can the ocean be colder than 0 degrees C, the temperature at which water freezes? As it turns out, the concentration of the particles (in this case, the ions from the salt) in ocean water lowers the temperature at which the saltwater will freeze. Students will learn how ocean water freezes at a lower temperature than freshwater by
This is a one hour webinar is part of the Polaris Project 2012, conducted by Max Holmes and John Schade. In this session Andy Bunn, professor at Western Washington University, presents a lecture on the history and science of climate change.
This is a one hour webinar specifically for the participants of the Polaris Project 2012, conducted by Max Holmes and John Schade. In this session, a variety of team members present their scientific work.
This presentation is part of the Polaris Project Webinar Series preparing participants for the field season 2012. This is one of two lectures to view for Session Two. You need to also watch the Sobczak Presentation Archive.
This presentation is part of the Polaris Project Webinar Series preparing participants for the field season 2012. This is one of two lecture to view for Session Two. You need to also watch the Schade Presentation Archive.
This is a one hour webinar specifically for the participants of the Polaris Project 2012, conducted by Max Holmes and John Schade. This is the introductory session.
Article describing teacher Laura Lukes' hands-on teaching experiences and her 2011 expedition with an international group of two dozen students at Kangerlussuaq Field School in Greenland.
A link to the Young Explores Grant and Program. Today, Young Explorers grants help cover field project costs for hard-working, passionate, creative individuals with great ideas. We focus on the disciplines we're known for, and also on emerging fields that matter most to understanding—and improving—the world we share.
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