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
When a bottle or can of carbonated beverage is opened the carbon dioxide is allowed gas to come out of solution. This is because there is a pressure differential between the carbon dioxide in the liquid and carbon dioxide in the air. The pressure in the liquid is higher than the pressure in the air so the carbon dioxide moves
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
Teacher Dave Jones and researcher Mike DeGrandpre present live from Montana discussing the research that took place for 4 weeks aboard the CCGS Louis S. St-Laurent looking at CO2 and pH Studies of the Arctic Ocean.
A short newspaper article featuring PolarTREC teacher Dave Jones in the 8/8/2017 issue of the Missoulian! He will set sail on 9/6/2017 aboard the Canadian Ice Breaker CCGS Louis S. St-Laurent with researcher Mike DeGrandpre heading for the Beaufort Sea.
PolarTREC alumna Susy Ellison talks about her two expeditions and how they affected her personally and professionally. Researcher Jeff Rasic joins in to talk about what it was like to have a teacher in the field for the Early Human Settlement in Arctic Alaska 2011 expedition.
Through this demonstration and review of the attached research documents and the expedition PolarConnect event archive you will better be able to visualize how warming deep ocean currents undermine the ice sheets of Antarctica.
Objectives
To determine, through a demonstration and review of a scientific abstract, how warm water currents speed up ice sheet loss and sub-ice
As a teacher on the NB Palmer Totten Cruise in the winter of 2014, I successfully traversed the Magnetic South Pole. This is a wandering point on the Earth’s surface where geomagnetic field lines are directed vertically upwards. As an Outdoor Educator I utilize compasses regularly to navigate. The traverse of the Magnetic South Pole inspired this lesson
This is part two of a small series following Parishville-Hopkinton Central School science teacher Glenn W. Clark’s involvement last winter in the National Science Foundation’s 2013-2014 Antarctic Research Consortium research trip to Eastern Antarctica. Since his return to the north country last spring, he has been educating the public about the excursion in a three piece presentation on science, expedition