The Dry Valleys Ecosystem project (a Long Term Ecological Research program - LTER) has been a continuous line of research since the inception of the McMurdo Dry Valley LTER since 1992. This project seeks to test hypotheses regarding the response of Antarctic biotic communities to changes in climatic conditions over time. I participated in the 30th
Teacher Bill Henske describes the science and fieldwork behind the Dry Valleys Ecosystem Study from McMurdo Field Station in Antarctica. This presentation took place on 24 January 2023.
Educator Kim Young and Researcher Christina Minions from the Winter Respiration in the Arctic Team discuss permafrost in Alaska and what climate factors are affecting it. This presentation was broadcast live from Weston, Massachusetts on 8 April 2019.
This resource is a 2-minute immersive video that takes students inside the Permafrost Research Tunnel outside of Fairbanks, Alaska. It includes footage of both the new and old sections of the tunnel.
Objectives
Through watching this video, students will get to see what permafrost looks like from the inside, identifying typical features geological features (ex. ice wedges). Through the
This lesson plan transports students to two field sites outside of Fairbanks, Alaska to investigate the interconnected relationships between climate change and permafrost. Students will use authentic field data from site photographs, soil temperature, and thaw depth measurements to draw inferences. An ESRI StoryMap, faux field journal, and 360 site images are used to engage students in the inquiry
PolarTREC is a teacher professional development program funded through the Arctic Research Consortium of the United States (ARCUS) and National Science Foundation (NSF). PolarTREC pairs middle and high school teachers with scientific research teams to allow them to “study-abroad” as a scientific team member authentically integrated into polar (Arctic or Antarctic) field science. The PolarTREC experience facilitates
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