This American Public Media Educate podcast features PolarTREC alumni, Melissa Lau. She talks about how her experiences in PolarTREC has influenced how she approaches teaching climate change in the classroom. Here's the link to the Education podcast:
Melissa Lau spent a month in the tundra ecosystem gathering data using a device called a Greenseeker. This device measures exactly how green a plant is by calculating its NDVI or Normalized Difference Vegetation Index. In this lesson, students will explore light waves, how they interact with plants, and find out how green is green.
PolarTREC, funded by ARCUS (Arctic Research Consortium of the United States) and the NSF (National Science Foundation), endeavors to connect educators and researchers in real field work experiences. Educators then take that experience back to their learners and community and share their experience in the form of lessons, lectures, and enhanced experiences in the classroom. As
PolarConnect event with teacher Melissa Lau and researchers Jeremy May and Matthew Simon discussing their research on Phenology and Vegetation Change in the Warming Arctic. This presentation was broadcast live from Toolik Field Station, Alaska on 20 June 2018.
PolarTREC teacher Jillian Worssam was one of a handful of teachers singled out by the Rodel Foundation of Arizona as an exemplary teacher. This article gives a sneak peak into Ms. Worssam's very hands-on, field-based classroom and how she connects with her middle school students.
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