InTeGrate Modules and Courses >Water Science and Society > Student Materials > Module 2: Climatology of Water > Water Distribution on Earth > Uneven Distribution
InTeGrate's Earth-focused Modules and Courses for the Undergraduate Classroom
showLearn More
These materials are part of a collection of classroom-tested modules and courses developed by InTeGrate. The materials engage students in understanding the earth system as it intertwines with key societal issues. The collection is freely available and ready to be adapted by undergraduate educators across a range of courses including: general education or majors courses in Earth-focused disciplines such as geoscience or environmental science, social science, engineering, and other sciences, as well as courses for interdisciplinary programs.
Explore the Collection »
show Download
The student materials are available for offline viewing below. Downloadable versions of the instructor materials are available from this location on the instructor materials pages. Learn more about using the different versions of InTeGrate materials »

Download a PDF of all web pages for the student materials

Download a zip file that includes all the web pages and downloadable files from the student materials

For the Instructor

These student materials complement the Water Science and Society Instructor Materials. If you would like your students to have access to the student materials, we suggest you either point them at the Student Version which omits the framing pages with information designed for faculty (and this box). Or you can download these pages in several formats that you can include in your course website or local Learning Managment System. Learn more about using, modifying, and sharing InTeGrate teaching materials.

Uneven Distribution

Why is water distributed unevenly across the Earth's surface?

As you probably know, things are far more interesting than a hypothetical case of evenly distributed precipitation! Both precipitation and evaporation vary widely over the Earth's surface. This unequal distribution of water on the planet drives a diversity in climate and ecosystems (or biomes); water availability for human life, industry, and agriculture; and is fundamentally and intimately tied to the history of politics, economics, food production, population dynamics, and conflict – both in the U.S. and globally.

The abundance of water in some areas and scarcity in others follows systematic and predictable patterns. As part of this module, we'll explore the physical processes that shape the overall distribution of precipitation - and thus water resources.

Learning Checkpoint

Note: The questions below are not graded. They may show up as summative evaluation questions on mid-term or final exams.

1) Look at Figure 7 above. What is the annual mean precipitation in Southern Nevada?

  1. 32 in/yr
  2. greater than 80 in/yr
  3. 0 in/yr
  4. 4-8 in/yr

2) Look at Figure 7 above. What is the annual mean precipitation in Coastal Washington State?

  1. a. 32 in/yr
  2. greater than 80 in/yr
  3. 0 in/yr
  4. 4-8 in/yr

3) Why do you think Nevada and Eastern Oregon are deserts?

  1. a. They are far North of the equator.
  2. They are far from the ocean.
  3. They are in the rain shadow of mountains.
  4. They are subject to large annual temperature fluctuations.
  5. They are at high elevation.

4) Look at Figure 8. What do you think is the global pattern of precipitation?

  1. a. It rains most South of the equator.
  2. There is East-West "banding" of climate/precipitation.
  3. There is North-South "banding" of climate/precipitation.
  4. There is snow in the Southern Hemisphere year-round.

Note the contrasting patterns in the two images in Figure 8 above, based on global satellite coverage. Vegetation in the southern hemisphere, which has relatively more ocean area (and less land area) than the northern hemisphere, changes little seasonally, whereas vegetation distribution in the northern hemisphere undergoes large changes. Why is that? There are probably two impacts on vegetation distribution—precipitation and temperature. Examine the figure below that illustrates the available moisture seasonally (summer vs. winter) and compare to the distribution of vegetation for the same seasons. Think about the role of temperature, precipitation, and soil moisture (water availability to plants), as well as the availability of sunlight for photosynthesis. Yes, there is a more complex relationship between plant growth and other factors, but the hydrologic cycle plays a major role.


These materials are part of a collection of classroom-tested modules and courses developed by InTeGrate. The materials engage students in understanding the earth system as it intertwines with key societal issues. The collection is freely available and ready to be adapted by undergraduate educators across a range of courses including: general education or majors courses in Earth-focused disciplines such as geoscience or environmental science, social science, engineering, and other sciences, as well as courses for interdisciplinary programs.
Explore the Collection »