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 activity was adapted from a TEA activity authored by:
* Sandra Kolb, Education Consultant, Poulsbo, Washington
* Kolene Krysl, Westside Community Schools, Omaha, Nebraska
* Larry Rose, Pleasanton Middle School, Pleasanton, California
* Wendy Slijk, La Costa Canyon High School, San Diego County, California
The original activity can be found at: http://tea.armadaproject.org/activity/kolb/tobesaltyseaiceornottobesaltyseaice_main.html
The website, Ice Stories, features short interviews and other interesting content live from the polar regions. This weblink has a short video interview of PolarTREC teacher, Craig Beals, while taking part in a PolarTREC expedition with Barry Lefer at Summit, Greenland.
PolarTREC Teacher, Craig Beals, talks about his experiences at Summit, Greenland in this online version of an article published by the Billings Gazette on July 21, 2008.
The Kuril Biocomplexity Project is a National Science Foundation-funded research project led by the University of Washington and being conducted by a team of American, Japanese and Russian scholars and students who are examining a 5000-year history of human-environmental interactions along the Kuril Island chain in the northwest Pacific Ocean. This is the link to the project website.
Students are presented with an actual series of tundra photos, which they use to develop a hypothesis for which sort of ground cover will have the most/least permafrost depth. Then they are given a set of actual data and use this to test their hypothesis
Objective
Students will:
* understand what permafrost is and how it develops