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.
PolarTREC educator Monica Nunez and researcher Dr. Craig Tweedie discuss the many projects that UTEP is involved in across the Barrow Peninsula. Collectively, these projects are helping to advance our knowledge of terrestrial, aquatic, coastal and marine ecosystem structure and function and how these systems are responding to arctic change. This event was broadcast live from a research boat outside
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
PolarConnect event with Heidi Roop who is working with an Ice Core Drilling team on the West Antarctic Ice Sheet in Antarctica. A PDF of the slides is not available for this event.