2011 Tsunami Propagation
Julie Ann Fero Martin, Hartnell College
This activity was selected for the On the Cutting Edge Reviewed Teaching Collection
This activity has received positive reviews in a peer review process involving five review categories. The five categories included in the process are
- Scientific Accuracy
- Alignment of Learning Goals, Activities, and Assessments
- Pedagogic Effectiveness
- Robustness (usability and dependability of all components)
- Completeness of the ActivitySheet web page
For more information about the peer review process itself, please see https://serc.carleton.edu/teachearth/activity_review.html.
- First Publication: May 28, 2013
- Reviewed: January 16, 2015 -- Reviewed by the On the Cutting Edge Activity Review Process
Summary
This activity uses data collected from DART (Deep-ocean Assessment and Reporting of Tsunamis) stations in the Pacific following the 2011 tsunami generated off the coast of Japan. Students are required to map the wave front after 5, 10, and 15 hours to better understand the speed and propagation of the tsunami wave.
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Audience
This activity is used in an introductory oceanography course for non-majors. The class meets once a week and does not have a lab component, so this activity is used to break-up the 3 hour lecture period.
Skills and concepts that students must have mastered
The preceding lecture should cover the difference between shallow-water and deep-water waves, provide a brief description of tsunamis, and discuss how these waves are formed and travel across the ocean. Students need to understand that the tsunami wave front propagates out in a roughly circular patter from the source location. Additionally, a general overview of how tsunami are recorded by the DART stations is useful. Students must also be familiar with contour plots and will need some direction on how to plot contours from discrete points.
How the activity is situated in the course
This is a stand-alone exercise that is situated in the middle of a short lecture on tsunami, which is part of a longer lecture on ocean waves and currents.
Goals
Content/concepts goals for this activity
Practice plotting information on a map and doing simple wave speed calculations.
Higher order thinking skills goals for this activity
Practice reading and interpreting information contained on a map. Synthesizing the information from lecture regarding the difference between shallow-water and deep-water waves to better understand how this relates to the speed of the tsunami wave front.
Other skills goals for this activity
Description and Teaching Materials
This activity uses data collected from DART (Deep-ocean Assessment and Reporting of Tsunamis) stations in the Pacific following the 2011 tsunami generated off the coast of Japan. Based on tsunami arrival times at each DART station, students are required to map the wave front after 5, 10, and 15 hours to better understand the speed and propagation of the tsunami wave. Students are required to estimate when the tsunami would arrive at various locations and then use these estimations to calculate the speed of the wave. At the end of the activity students should understand how tsunami waves propagate across the ocean (roughly circular trajectory), that tsunami are shallow water waves and what this means for calculating the wave speed, and that tsunami, like all waves, are a propagation of energy.
Teaching Notes and Tips
I have found that my students have some trouble plotting the data because they have an incomplete understanding of the concept of a "wave-front." Thoroughly describing this term using examples before the exercise helps.
Assessment
I listen to the individual groups during the exercise and then lead a full class discussion to qualitatively assess the students' understanding of the assignment. I also collect the assignment from each student to catch any persisting misconceptions after the discussion.
References and Resources