There is a plausible explanation for how carbon dioxide molecules could interact with water molecules thereby forming a solution where the carbon dioxide is the solute and water is the solvent (as it usually is). The weak inter-molecular attractive forces rely on the polarity of the water molecule and the high density of electrons at either end of the
I spent a month on a boat in the Arctic as part of the 28 member Science Team that lived and worked alongside the 53 member Crew of the Canadian Coast Guard Ship Louis S. St. Laurent, a 392 foot icebreaker out of St. John's, Newfoundland
PolarTREC teacher Elizabeth Eubanks traveled to the Alaska Marine Science Symposium with her students. They presented a poster about their experience as her students.
The following presentation was given by Dr. Patricia Yager at the 2012 Arctic Ocean Ecosystem Workshop in Barrow, Alaska. The presentation outlines Dr. Yager's work in biological and chemical oceanography, and focuses on the feedbacks between climate change and marine ecosystems at different locations around the world.
Teacher Elizabeth Eubanks recently returned from a research trip to Costa Rica along with Steve Oberbauer, a professor of biological sciences at Florida International University. In 2008, they had traveled to Barrow, Alaska to study the role of global warming on Arctic ecosystems as part of a PolarTREC exition. In Dr. Oberbauer's words, "Elizabeth was so good in Alaska, I
This data plotting lesson compares different stratospheric ozone data collected at the South Pole in September 1969, September 1998, September 2008, January 1999, and January 2008. This ozone comparison activity allows students to make conclusions about the annual and seasonal ozone hole as well as overall ozone concentration changes over Antarctica. Students use authentic data collected at the
This data plotting lesson is about temperature changes throughout the atmosphere. The data was collected together with the ozone data in January 2008.
The temperature vs. altitude profile allows students to make conclusions about annual and seasonal temperature changes in the atmosphere up to about 35 kilometers in the stratosphere. The best part of this lesson is using
This is presentation provides an overview about sea ice in Antarctica as presented by Dr. Patricia Yager. She has slides about the daylight and seasons and related sea ice concentrations. She also has several slides about sea ice as a habitat and about the types of organisms associated with the sea ice. The main part of this presentation focuses on