T21 Identifying and Addressing K–16 Student Misconceptions in the Earth-Science Classroom
Sunday, 9 October 2011
8:00 AM - 12:00 PM
Room 211AB
LESSONS AND APPLICATIONS FROM COMPLEXITY THEORY TO THE GEOSCIENCES
Paper number: T21-14
Program: Technical Sessions
Time: 11:15 AM – 11:30 AM
Authors
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Steve J. BaedkeJames Madison University, Harrisonburg, VA
Abstract
Based on Turcotte (1997 and 2006) and Fichter et al. (2010), we propose that to understand Complex Earth Systems, one’s thinking must minimally be prepared and trained to reflexively presume and search for the following properties. The more energy/information a system dissipates: 1) the more complex it becomes–entropy goes down (i.e. order increases); 2) the more sensitive dependent it becomes, capable of dramatic evolutionary change from minuscule changes in input; 3) the faster the changes come; 4) the larger the changes become, following a power law. Furthermore, 5) despite being deterministic these systems are inherently unpredictable; the behavior often appears random; 6) yet, these systems produce readily recognizable and repeatable patterns (e.g. ripples) following simple algorithms.
In the geosciences, models and examples that systematically document the role and expression of these outcomes are still poorly developed. We have developed and assessed 2 classes at JMU that teach Complex Earth Systems as non-equilibrium complex systems. This poster presents the principles necessary to recognize the Earth as a complex system, and illustrates examples where they can be readily recognized.