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.
This PolarConnect event was conducted with PolarTREC teacher Claude Larson, and members of the research team that she worked with on the Prehistoric Human Response to Climate Change 2010 project in Kamchatka, Russia.
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