Earth System Topics: Oceans
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NanTroSEIZE in 3-D
Donald Reed, San Jose State University
We have developed a web-based virtual expedition, NanTroSEIZE in 3-D, based on a seismic survey associated with the NanTroSEIZE program of NSF-MARGINS and IODP to study the properties of the plate boundary fault ...
Poleward Heat Transport Jigsaw
E. Christa Farmer, Hofstra University
Based on great plate tectonic exercise by Sawyer et al. (2005 JGE), this small-group exercise with maps of data about earth's energy balance helps students visualize poleward heat transport.
Jennifer Bown, Clackamas Community College
Students choose shell fragments from different species of Molluscs and calculate percent lose after soaking in different ph solutions for different periods of time. They research ocean acidification and especially ...
Confirmation of the IPCC Prediction re: Increased Storminess
Robert Kuhlman, Montgomery County Community College
A two-part culminating activity for a meteorology/climatology unit in an Earth Science course centered upon data acquisition and analysis regarding the confirmation of the IPCC predicition regarding increased ...
Is There a Trend in Hurricane Number or Intensity?
Todd Ellis, Western Michigan University
This lab guides students through an examination of the hurricane record to determine if there is a trend in hurricane intensity over the past 40 years and introduces some issues related to statistics and ...
Estimating Exchange Rates of Water in Embayments using Simple Budget Equations.
Keith Sverdrup, University of Wisconsin-Milwaukee
Simple budgets may be used to estimate the exchange of water in embayments that capitalize on the concept of steady state and conservation principals. This is especially true for bays that experience a significant exchange of freshwater. This exchange of freshwater may reduce the average salt concentration in the bay compared to seawater if it involves addition of freshwater from rivers, R, and/or precipitation, P. Alternatively, it may increase the average salt concentration in the bay compared to seawater if there is relatively little river input and high evaporation, E. Since freshwater input changes the salt concentration in the bay, and salt is a conservative material, it is possible to combine two steady state budgets for a bay, one for salt and one for water, to solve for the magnitude of the water flows that enter and exit the bay mouth. Students will make actual calculations for the inflow and outflow of water to Puget Sound, Washington and the Mediterranean Sea and compare them to actual measured values.
Using Google Earth to measure seacliff erosion rates
Alfred Hochstaedter, Monterey Peninsula College
This lab uses Google Earth to measure the rate of seacliff retreat. It touches upon coastal processes, natural hazards, and coastal management issues. The central focus of the lab is in the Monterey Bay area.
Student Lead Discussions: Articles from the Literature and Final Writing Assignment
Dave Dempsey, San Francisco State University
This is a two-stage assignment. The first stage is a student-led discussion of a set of closely related articles selected by the instructors from the climate change literature. The second stage is an 8-12 page ...
Exercise 5: The human impact of sea level changes, plus extensions to impacts of other natural events on human populations
Barb Tewksbury, Hamilton College
Barbara and David Tewksbury, Hamilton College Summary In this eight-part exercise, students download NOAA high resolution bathy/topo DEMs and TIGER census data to predict the location of shorelines, the extent of ...
Tsunami Travel Time Approximation
Eric Grosfils, Pomona College
Eric Grosfils, Pomona College Summary Students are asked to calculate approximate tsunami travel times across the Pacific basin. The assignment builds off of a lab introducing students to Spatial Analyst, and ...