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Cryosphere

Mountain Environments Advanced On-Line Activity

Introduction

The term "cryosphere" traces its origins to the Greek word kruos for frost. It collectively describes the portions of the earth's surface where water is in a solid form such as sea ice, snow cover, glaciers, ice caps and permafrost. The relationship between snow water equivalent and water availability to rivers and streams is of paramount importance to the western United States. This area is typically arid and agriculture depends on irrigation. A large proportion of this water comes from melting snow that accumulated in the mountains of the region over the winter, and enters rivers and streams as melt-water in the spring and early summer.

Learner Outcomes

By completing this lesson, students will:

Teacher's Notes can be found by clicking here.

Activity
 
A. From the map above, identify the major drainages in the western United States. (Columbia, Colorado, Missouri, Sierra-Nevada). Click on the map to see a larger version. 
B. Run the animation called Snow Water Equivalent(SWE). (Most Current Image) After viewing the animation, answer the following questions.

C. Run the animation Deviation from Normal Snow Water Equivalent. Assessment and Extension Ideas

1. Have students go to specific sites on the internet and download precipitation images.

2. After students observe animation on snow water equivalent, predict areas of flooding or drought.

3. Check predictions for accuracy from the internet sites used in in the activity.

4. Go to Other Cryosphere Internet Sites and look for connections between snow and ice accumulation and water availability.

Other Cryosphere Internet Sites

Cryospheric System (CRYSYS)

Canadian Ice Service

Northwest River Forecast Center Snow Information

National Snow and Ice Data Center

Polar Science Center

North Atlantic and Pacific Vessel Icing Forecasts

West Antarctic Sheet Ice Initiative

British Antarctic Survey

NCEP OMB Sea Ice Home Page