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
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
This PolarConnect event was conducted with PolarTREC teacher Claude Larson, and members of the research team that she worked with on the Prehistoric Human Response to Climate Change 2010 project in Kamchatka, Russia.
This Live from IPY! Event was was held with Lindsay Knippenberg who discussed her recent research on the Microorganisms in Antarctic Glacier Ice expedition in the Dry Valleys.