Lake Powell, Utah
acquired March 25, 1999 download large image (997 KB, JPEG, 2154x2154)
acquired March 25, 1999 download GeoTIFF file (10 MB, TIFF, 2154x2154)
Lake Powell, Utah
acquired April 2, 2005 download large image (1 MB, JPEG, 2154x2154)
acquired April 2, 2005 download GeoTIFF file (12 MB, TIFF, 2154x2154)
acquired 1999 - 2013 download Google Earth file (KML)

In southern Utah, the Colorado River, halted by Arizona’s Glen Canyon Dam, creates Lake Powell, a meandering, narrow reservoir that follows the contours of the river. In the early twenty-first century, this modern marvel of engineering faced an ancient enemy: severe, prolonged drought in the American Southwest. Combined with water withdrawals that many believe are not sustainable, the drought has taken its toll on Lake Powell water levels.

NASA’s Landsat 5 satellite captured these natural-color images on March 25, 1999 (top), and April 2, 2005 (bottom). Both images show the northeastern reaches of Lake Powell, where it fills Glen Canyon and connects with the Colorado and Dirty Devil Rivers (at normal water levels, both rivers are drowned by the lake). The southward-reaching finger of land in the right half of each image is Mille Crag Bend, and the Colorado River flows around the bend’s southern perimeter en route to Lake Powell. Sunlight brightens plateaus and southeast-facing slopes, casting shadows on the northern and western faces of this rugged landscape.

In the image acquired on March 25, 1999, water levels in Lake Powell appear normal. The main body of Lake Powell and the branch into Dirty Devil Canyon are dark blue. Flowing into Lake Powell, the Colorado River appears green-brown, indicative of sediment-rich water. The image from April 2, 2005, however, shows a vastly different situation. In this image, Lake Powell’s water levels have dropped so much that the northwestern side branch of the reservoir (called North Wash) has been isolated from the main water body. In the main body of Lake Powell, water pools along its eastern edge while the western portion shows large expanses of dry canyon floor. Narrow Canyon and Dirty Devil Canyon appear in earth tones. (At low water levels, the Dirty Devil River can be too narrow for Landsat to detect.)

Lake Powell’s water levels plummeted in 2005, according to the U.S. Department of the Interior Bureau of Reclamation. Water levels recovered somewhat over the next two years, but dry conditions struck again in 2008. For a time series of Lake Powell images from 1999 to 2009, see the Earth Observatory feature World of Change: Lake Powell.

  1. References

  2. Committee on the Scientific Bases of Colorado River Basin Water Management, National Research Council. (2007). Colorado River Basin Water Management: Evaluating and Adjusting to Hydroclimatic Variability. National Academies Press. Accessed May 7, 2009.
  3. Earth Observatory. (2004, December 12). Glen Canyon Dam. Accessed May 6, 2009.
  4. Earth Observatory. (2007, October 17). Water Levels in Lake Powell. Accessed May 6, 2009.
  5. Earth Observatory. (2009, March 30). Spring Snow Brings Moisture to Colorado Front Range. Accessed May 6, 2009.
  6. Stokstad, E. (2007, February 21). Western drought: The worst is yet to come. ScienceNOW. Accessed May 6, 2009.
  7. U.S. Department of the Interior Bureau of Reclamation. Upper Colorado Region Water Operations: Current Status: Lake Powell. Accessed May 6, 2009.
  8. Wikipedia. (2009, May 3). ColoradoRiver. Accessed May 6, 2009.

Image by Robert Simmon, based on data provided by the Landsat 5 science team. Caption by Michon Scott and Rebecca Lindsey.

Instrument(s): 
Landsat 5 - TM

Lake Powell, Utah

May 13, 2009
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