Use a topographic map to deliniate a watershed, draw a map bar …
Use a topographic map to deliniate a watershed, draw a map bar scale, and calculate a map ratio scale.
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Students pose a question that can be answered using the SEM and …
Students pose a question that can be answered using the SEM and sand they have previously collected from beach profiles.
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Maps displaying global environmental data (specifically Solar Energy and Average Temperature) through …
Maps displaying global environmental data (specifically Solar Energy and Average Temperature) through the course of a year are compared in order to understand how the Earth works as a system focusing on Polar Regions. Students then explore data from schools located in Alaska and Antarctica to understand processes that drive the temperature patterns; students then visit the National Snow and Ice Data Center Web site to learn more about the Cryosphere (focusing on Albedo and Sea Ice); finally students visit NOAA's web site looking at data of Sea Ice data anomalies. (Link to the relevant pages in these web sites are listed below.)
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In this exercise students work with light, temperature, and phytoplankton biomass proxy …
In this exercise students work with light, temperature, and phytoplankton biomass proxy (chlorophyll a concentration) data to;
Become more skilled in reading and interpreting semi log graphs, temperature profiles, and time series plots. Practice unit conversions. Gain an understanding of k, the attenuation coefficient for nondirectional light. See how the depth of the photic zone and the surface mixed layer varies seasonally at temperate latitudes and how this relates to seasonal phytoplankton productivity dynamics.
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Use a Slinky to show:P and S waves, Wave reflection, and Standing …
Use a Slinky to show:P and S waves, Wave reflection, and Standing waves in interactive lecture demonstration.
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This physical model presented by Jeffrey S. Barker, Associate Professor of Geophysics, Pennsylvania State University. Starting Point page organized by R.M. MacKay.
Light is our usual method for observing on land, but water quickly …
Light is our usual method for observing on land, but water quickly absorbs light making it less useful in the ocean. On the other hand, sound in water can travel long distances before it is absorbed to the point where it becomes inaudible. For this reason sound is frequently used to "see" in the ocean, as when scientists map the sea floor. In this activity students work with sound and light data. In the process they come to appreciate that several factors affect the speed of sound --salinity, temperature and pressure -- and learn how to calculate sound intensity at a distance from the source. By plotting sunlight intensity versus depth in the ocean students learn that light is quickly absorbed in water. Students also read graphs, make calculations, and interpret both. They view two videos and may listen to underwater sounds (see reference section below for a link to a sound gallery). They read a short article on the changing soundscape in the ocean in modern times. These activities provide an engaging, varied look at sound and light in the ocean.
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This is an in-class activity. I used it relatively early in the …
This is an in-class activity. I used it relatively early in the semester, after covering the basic water properties portion of the class. I use the relationship between temperature/salinity/density to begin discussing vertical movement of water. The first purpose of this activity is to reinforce the concepts that have just been explained about the relationship between temperature and density and salinity and density. The second purpose is to bring these ideas back to what they have learned about density differences. Finally, the activity is also designed to help them learn how to read graphs.
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The topographic map exercise uses tools that the students may have had …
The topographic map exercise uses tools that the students may have had some exposure to, surface maps, and forces them to view it in a more critical manner. They are asked to use maps of different types and representing different landscapes to answer a series of questions. It teaches them to identify the information the map provides and to read the topographic contours to understand how they relate to the real-world surface. The principles of interpolation and contouring are addressed as students create their own topographic map from a set of elevation points. Students are introduced to the idea of a topographic profile, which they will be using throughout the course in later lab exercises and field experiences.
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This lab has two purposes. First, it introduces students to topographic maps …
This lab has two purposes. First, it introduces students to topographic maps (including latitude/longitude, map scales, contour intervals, and relief). Second, it introduces students to a river system that they will be studying throughout the semester, and begins preparing students to collect and analyze data from the field. The topographic maps are used to look at topographic characteristics of the river, such as its gradient and its longitudinal profile.
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Part 1 The SAGUARO Exploring GIS Investigations for Earth Science curriculum requries …
Part 1
The SAGUARO Exploring GIS Investigations for Earth Science curriculum requries the use of ESRI's ArcView GIS software version 3.0 for Macintosh or 3.2 and higher for PC. Use ArcGIS and data files from the SAGUARO Project's (http://pro.arcgis.com/en/pro-app/help/projects/supported-data-types-and-items.htm) Exploring Tropical Cyclones investigations. After the students are introduced to the program they are asked to determine what criteria are required for the formation of tropical cyclones. Exploring Tropical Cyclones Unit 1 has a great deal of data for the students to use. The data is presented as layers on a world map. Different features can be turned on and off at will, and layers can be brought in from other units if desired.
Features they can work with are:
August SST February SST tropical cyclone tracks locations of tropical cyclone formation for Jun-Sep locations of tropical cyclone formation for Dec-Mar
Part 2
Students are divided into small groups (3-4 students works well) where they compare their findings (including what evidence they used) with the findings of the other group members. Each group is then asked to determine the threshold temperature for tropical cyclone formation as well as to calculate the area of the ocean that has SST equal to or above this threshold temperature (you can have them calculate this for each season, or as a total area including both February and August data).
Part 3
Class discussion of what they have found so far. Introduce them to model predictions of SST for different atmospheric CO2 levels. Propose a 2 degree C increase in tropical SST and ask what they think that will mean. What other factors might influence the formation of tropical cyclones?
Part 4
Assign an article or two (ideally a published peer reviewed article - to introduce them to this type of scientific writing - that is if you can find one that you consider appropriate for your students) that introduces them to other factors required for tropical cyclone formation and predictions of how climate change might affect them. For example an article that discusses the role of wind speed near the surface of the ocean, or vertical wind shear, or one that shows that the threshold temperature is actually predicted to increase by the same magnitude as the SST increase. Have them write a report that summaries the criteria for cyclogenesis as well as explaining how they would go about predicting where tropical cyclones will form as a result of an increased SST. They do not need to perform all of the tests they propose! They should state what sort of information they would like to obtain and why.
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In this activity, students are introduced to the concept of ecosystem services, …
In this activity, students are introduced to the concept of ecosystem services, provided with a tool for exploring these services in particular landscapes, and led through a few examples so that they will be comfortable using the tool. Google Earth is presented as a tool for exploring landscapes and evaluating the ecosystem services provided by those landscapes, including spatial and temporal variability. Students use Google Earth to identify and classify ecosystem services according to the Millennium Ecosystem Assessment (MA) categories, first by looking at an example landscape along the the Missouri River, and then by looking at an example specific to their location.
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In this activity, students focus on ecosystem services specifically related to the …
In this activity, students focus on ecosystem services specifically related to the hydrologic cycle. Using rainfall-runoff data for a small watershed in Ohio, students are introduced to the technical vocabulary associated with watersheds, watershed hydrology, and water balance. Working with hydrologic data will enable the students to test their understanding of watershed hydrology and the water balance equation, which is a measure of how much water is stored within different parts of the watershed.
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In this activity, students examine the impact of land use on runoff. …
In this activity, students examine the impact of land use on runoff. Using rainfall-runoff data for two small watersheds in Ohio, one dominated by agricultural land uses and the other dominated by urban land uses, students evaluate natural and human factors that impact watershed hydrology and water balance, and generate potential provisioning and regulating services provided by natural ecosystems within watersheds.
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In this opening unit, students develop the societal context for understanding earthquake …
In this opening unit, students develop the societal context for understanding earthquake hazards using as a case study the 2011 Tohoku, Japan, earthquake. It starts with a short homework "scavenger hunt" in which students find a compelling video and information about the earthquake. In class, they share some of what they have found and then engage in a series of think-pair-share exercises to investigate both the societal and scientific data about the earthquake.
Show more about Online Teaching suggestions Hide Online-ready: This opening class discussion about earthquakes and societal impacts could easily be converted to an online discussion format.
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This unit introduces students to Structure from Motion (SfM). SfM is a …
This unit introduces students to Structure from Motion (SfM). SfM is a photogrammetric technique that uses overlapping images to construct a 3D model of the scene and has widespread research applications in geodesy, geomorphology, structural geology, and other subfields of geology. SfM can be collected from a hand-held camera or an airborne platform such as an aircraft, tethered balloon, kite, or UAS (unmanned aerial system). After an introduction to the basics of SfM, students will design and conduct their own survey of a geologic feature, followed by an optional (but highly encouraged) introductory exploration of SfM data after returning from the field.
Show more about Online Teaching suggestions Hide Online teaching: This unit was adapted to an online remote field teaching activity. Getting started with Structure from Motion (SfM) photogrammetry (remote field collection).
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Field experience using geodetic and geophysical tools provides a unique opportunity for …
Field experience using geodetic and geophysical tools provides a unique opportunity for upper-level undergraduates to learn research skills applicable to their future graduate research or career path. This unit introduces students to terrestrial laser scanning (TLS), a ground-based, remote-sensing tool that generates three-dimensional point clouds, that has widespread research applications in geodesy, geomorphology, structural geology, and other subfields of geology. After an introduction to the basics of TLS, students will design and conduct their own survey of a geologic feature, followed by an optional introductory exploration of TLS data after returning from the field.
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In this activity, students model the impact of land-cover changes on stormwater …
In this activity, students model the impact of land-cover changes on stormwater runoff using the EPA's National Stormwater Calculator (Calculator). The students are introduced to the Calculator through a tutorial. Students are provided with a particular site -- a residential neighborhood -- and model two land-use scenarios associated with it: (1) a pre-expansion scenario that includes current forest and developed land cover, and (2) a post-expansion scenario, under which the forest cover will be developed as low-intensity residential.
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In this activity, students model the impact of changes in land cover …
In this activity, students model the impact of changes in land cover on stormwater runoff using the EPA's National Stormwater Calculator. Students mitigate increased stormwater runoff resulting from development with low impact development (LID) controls. Students assess the LID controls in terms of the ecosystem services that they are intended to replace and discuss alternative development designs to reduce the need for them.
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In this activity, students model the impact of a proposed land-use change …
In this activity, students model the impact of a proposed land-use change for a local site using the EPA's National Stormwater Calculator (Calculator). Given a description of the proposed land-use change, students devise and execute a series of simulations in the Calculator that model its potential impact on stormwater retention. Using additional simulations, students explore changes to the site that utilize low impact development (LID) controls to mitigate stormwater runoff.
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Geodetic survey techniques, such as TLS and SfM featured here, have many …
Geodetic survey techniques, such as TLS and SfM featured here, have many applications in sedimentology research, including lithological identification and analysis, sediment surface topography, and sequence stratigraphy. In this unit, students will design a survey of a geologic outcrop to conduct a sequence stratigraphy analysis. After conducting the survey in the field, students will analyze the parasequences found within the outcrop by mapping and measuring section thickness in the point cloud. The goal is to calculate deposition duration and sedimentation rate based on thicknesses extracted from the data.
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