Teaching Notes

Example Output

Example Output
Map and output from FieldScope GIS. Click the image for a larger view.

This example shows three different views of the United States created from FieldScope GISeach from the Globe Watersheds Module 1: Annual Evaporation, Annual Surface Runoff, and Annual Precipitation.

Grade Level

This chapter is appropriate for students in grades 6 through 12.

Learning Goals

After completing this chapter, students will be able to:

  • understand the Earth system processes that influence the rate and timing of evaporation and surface runoff in a given area;
  • compare annual precipitation patterns to annual evaporation and surface runoff patterns;
  • gain skill and understanding in the use of the GIS analysis tools, specifically the FieldScope Web GIS;
  • collect and record quantitative data in a data table and use it to support responses to questions; and
  • analyze and interpret data displayed on maps.

Background Information

Because precipitation and evaporation are components of the global water cycle, the total amount of water is constant over time with equal rates of precipitation and evaporation world-wide, but depending on location and time of year (i.e. seasons) these two may not balance with evaporation actually being greater than the precipitation. Students will explore precipitation and evaporation amounts across the U.S. As they collect data for study cities, they should recognize that there is not always a balance between the two components at a specific location. Some of the imbalance is the result of seasonal factors. For example, when precipitation occurs as snow during the winter, it doesn't contribute to surface runoff and evaporation as readily as when it melts during the spring. But, some of the imbalance may be due to the fact that there are regional or global factors involved.

Evaporation

Evaporation is a physical process by which a liquid or solid substance is transformed to the gaseous state. Evaporation represents the return of precipitation back into the atmosphere. Like precipitation, evaporation is not evenly distributed by location. The main sources of water vapor in the lower atmosphere are evaporation from Earth's surface and transpiration by plants.

Major factors influencing the rate of evaporation include atmospheric temperature, wind, atmospheric humidity, and the availability of water. Other contributing conditions and factors may include the following:

  • The movement of water between Earth's surface and the atmosphere is partially controlled by atmospheric humidity.
  • If there is little or no surface water, then the total amount of evaporation is low. In hot arid areas, such as the southwest, the total amount of evaporation is low because there is little water in the system to evaporate. However, the rate of evaporation (verses total amount of evaporation occurring over time) is high when water is available in hot arid areas. High evaporation is dependent on high precipitation, although there is sometimes a time lag in evaporation. For example, evaporation rates are high in the Pacific Northwest and Rocky Mountains in the spring and summer when there is little precipitation.
  • The type of land surface and vegetation influences evaporation and evapotranspiration rates.
  • The higher the wind speed, the greater the rate of evaporation.
  • Evaporation rates increase with increasing temperature.
  • During warmer months, plant evapotranspiration rates increase.

Surface Runoff

Surface runoff is the water that flows down creeks, streams and rivers. Precipitated water that has not evaporated back into the atmosphere or infiltrated into the ground runs off as surface water.

Major processes and factors influencing the timing and quantity of surface runoff include the amount of precipitation, rate of precipitation, form of precipitation (snow, rain, sleet, hail, etc), season the precipitation fell, infiltration rate, degree of ground saturation, land use and ground cover, and geology.

Instructional Strategies

Before the students begin this investigation, ask them to develop a working hypothesis describing the relationship between total annual precipitation and total annual evaporation. Will areas with high precipitation have high evaporation rates? Will areas with low precipitation, such as the hot, arid west, also have high total annual evaporation? Write the various hypotheses down on the class whiteboard so that students can refer back to them as they work through the GIS analysis.

As part of this investigation, students fill out a table of annual precipitation, evaporation, and surface runoff, for four pre-selected cities as well as three of their choice. One extension of this activity is to graph the data using Excel or other graphing/charting program. The chart can help students visualize the relationships of these different variables across the country. One important relationship for them to observe is how little surface runoff occurs compared to evaporation.

An Excel spreadsheet has been created for this purpose. Click here to download: Water_Availability.xls (Excel 40kB Sep22 09) After downloading and opening, click on the Investigation III tab at the bottom of the sheet to open the appropriate table and chart. Blank cells are in the table for students to add their selected cities. Below is an example of the data from the four pre-selected cities in the Investigation.

Another option is to have students create the chart on graph paper.

Excel_graph.jpg

Science Standards

The following National Science Education Standards are supported by this chapter:

Grades 5-8

Science as Inquiry

  • 8ASI1.3 Use appropriate tools and techniques to gather, analyze, and interpret data.
  • 8ASI1.4 Develop descriptions, explanations, predictions, and models using evidence.

Earth and Space Science

  • 8DESS1.6 Water, which covers the majority of Earth's surface, circulates through the crust, oceans, and atmosphere in what is known as the "water cycle."
  • 8DESS1.10 Global patterns of atmospheric movement influence local weather.
Grades 9-12

Science as Inquiry

  • 12ASI1.3 Use technology and mathematics to improve investigations and communications.

Earth and Space Science

  • 12DESS2.2 Movement of matter between reservoirs is driven by Earth's internal and external sources of energy.

Science in Personal and Social Perspectives

  • 12FSPSP3.1 Human populations use resources in the environment in order to maintain and improve their existence.
  • 12FSPSP4.1 Natural ecosystems provide an array of basic processes that affect humans.

Geography Standards

The following U.S. National Geography Standards are supported by this chapter:

The World in Spatial Terms

1. How to use maps and other geographic representations, tools, and technologies to acquire, process, and report information from a spatial perspective

Physical Systems

7. The physical processes that shape the patterns of Earth's surface

The Uses of Geography

18. How to apply geography to interpret the present and plan for the future

Other Standards

The following National Technology Foundation Standards are supported by this chapter:
  • Technology productivity tools. Students use technology tools to enhance learning, increase productivity, and promote creativity.
  • Technology problem-solving and decision-making tools. Students use technology resources for solving problems and making informed decisions.

Time Required

Up to 1 hour