Students will be able to:
* Analyze graphical data to draw conclusions
* Compare and contrast the chemical structures of nitrous oxide and carbon dioxide
* Explain how differences in the structure of nitrous oxide and carbon dioxide lead to differences in their reactivity and functions as a greenhouse gas
* Argue how changing shrubbery impacts climate change
Students will be able to:
* Graph, analyze, and predict data
* Develop claim, evidence, and reasoning
* Explain how permafrost is made, current conditions, and its impacts on climate and humans
Preparation
* This lesson plan can be taught either in the classroom or virtually online. Instructions on how to teach both ways are given in the Procedure
It’s sometimes a common and depressing comment to hear from your students, “I’ll never use this in my life! Teach me something practical like how to pay my taxes!” As teachers, we strive to make learning relevant to student’s lives, but for a multitude of reasons sometimes your lessons just don’t have that
PolarTREC teacher Andrea Skloss’ lesson was inspired by her Chukchi Sea Ecosystem Study aboard the USCGC Healy. In order to understand why this area is a biological hot spot of productivity, scientists must study components such as the trophic levels and more.
Objectives
In organisms and environments, the student knows that interdependence occurs among living systems and the environment
Journal article about Lesley Urasky's PolarTREC expedition, Glacial History in Antarctica, published in "In the Trenches", the news magazine of the National Association of Geoscience Teachers.
An article about Lesley Urasky's PolarTREC expedition, Glacial History in Antarctica during the 2010-2011 research season that appeared in the University of Wyoming's Alumnews.
The long-term objective of PolarTREC teacher Lesley Urasky's expedition research in Antarctica (Glacial History in Antarctica) is to determine the rate at which glaciers have receded since the Last Glacial Maximum. This lesson is designed to give students an understanding of the Last Glacial Maximum, the climatic conditions that lead to glacial periods, and how the rate of glacial