This content has been created with the intent for the teacher to develop it to best suit their classroom setting. In its most basic form, students are asked to analyze wet and dry berry data to determine how water content changes (or doesn’t) for several berry species over the course of one season.
This lesson has multiple stages or
The night before I left Alaska I stayed up chatting with some of the scientists in the Toolik dining hall talking about my return to “normal civilization”. We spoke about the little habits that you pick up while at the field station and aren’t sure you’re going to let go (wearing sunglasses 24/7) as well as
This is the archive of the PolarConnect event with teacher Liza Backman and the team from the Phenology and Vegetation in the Warming Arctic 2021 expedition who presented live from Toolik Field Station in Alaska on 15 June 2021.
News article on teacher Liza Backman and her experiences preparing for a trip to the Arctic to work on the phenology of arctic plants in a warming climate.
Educator Allyson Woodard and the Permafrost & Community Team discuss permafrost and how members of the community of Telida are helping to collect data to study the science of permafrost in their Alaskan village. This presentation was broadcast live from the Oregon Museum of Science and Industry (OMSI) in Portland, Oregon on 28 March 2019.
PolarTREC, funded by ARCUS (Arctic Research Consortium of the United States) and NSF (the National Science Foundation), brings educators to Polar Regions for immersive field work with researchers. This professional development opportunity allows educators to share real world experience with polar science in their communities, in the form of outreach and education. As an exhibit developer who
PolarTREC teacher Jacquelyn Hams' expedition is featured in Foundations: the Newsletter of the Geo2YC division of the National Association of Geoscience Teachers.
Even in Antarctica ice will melt. As the sun stays higher and higher in the sky as summer progresses, the warm sun causes the ice to melt. The questions that we are going to ask are: 1) Does clean ice (no sediment) or dirty ice (has sediment mixed in it) melt faster? and 2) Would the ice melt if
We know that we have lots of microorganisms growing where we live, but can microorganisms like bacteria also live in the harsh, cold, dry climate of Antarctica? Part of our research project in Antarctica is looking at the microorganisms that live in the Taylor Glacier. We are taking dirty ice (ice with lots of dirt/sediment in it) and
For this experiment, we are going to melt dirty ice (ice with lots of sediment/dirt in it) and clean ice (ice without sediment) from the Taylor Glacier. After we melt the ice, we are going to test the melt water for pH and conductivity, and then determine how much salt is actually in our ice samples. There are