Whitney Glacier Explained

Whitney
Type:Mountain glacier
Location:Mount Shasta,
Siskiyou County, California, United States
Map:USA California#USA
Label Position:right
Map Size:225
Coordinates:41.4139°N -122.2114°W
Coordinates Ref:[1]
Area:0.5sqmi
Length:2miles
Thickness:126feet in 1986
Terminus:Moraine
Status:Expanding

The Whitney Glacier is a glacier situated on Mount Shasta, in the U.S. state of California.[2] [3] The Whitney Glacier is the longest glacier and the only valley glacier in California. In area and volume, it ranks second in the state behind the nearby Hotlum Glacier. In 1986, the glacier was measured to be 126feet deep and over three km in length.[4] The glacier starts on Mount Shasta's Misery Hill at 13700feet and flows northwestward down to the saddle between Mount Shasta and Shastina,[5] where uneven ground causes a major icefall at 11800feet.[5] It then flows down the valley between the two peaks, reaching its terminus at 9500feetto9800feetft (toft).[5] [6]

Advance

In 2002, scientists made the first detailed survey of Mount Shasta's glaciers in 50 years. They found that seven of the glaciers have grown over the period 1951–2002, with the Hotlum and Wintun Glaciers nearly doubling, the Bolam Glacier increasing by half, and the Whitney and Konwakiton Glaciers growing by a third.[7] The study concluded that though there has been a two to three degree Celsius temperature rise in the region, there has also been a corresponding increase in the amount of snowfall. Increased temperatures have tapped Pacific Ocean moisture, leading to snowfalls that supply the accumulation zone of the glacier with 40 percent more snowfall than is melted in the ablation zone. Over the past 50 years, the glacier has actually expanded 30 percent, which is the opposite of what is being observed in most areas of the world. Researchers have also stated that if the global warming forecast for the upcoming next 100 years are accurate, the increased snowfall will not be enough to offset the increased melting, and the glacier is then likely to retreat.[8] [9]

Whitney Glacier, along with the Hubbard Glacier in Alaska, are larger now than in 1890.[10] However, Hubbard Glacier, along with a few other notable glaciers whose termini are at sea level, are calving glaciers.

See also

References

Notes and References

  1. 269049. Whitney Glacier. 2012-09-30.
  2. Web site: Existing Glaciers of Mount Shasta . College of the Siskiyous. 2007-01-23 .
  3. Web site: Glaciers of California. Glaciers of the American West. Glaciers Online. 2007-01-23 . https://web.archive.org/web/20060903035748/http://glaciers.research.pdx.edu/california.php . 2006-09-03.
  4. Web site: Driedger . Carolyn L. . Kennard, Paul M. . Ice volumes on Cascade volcanoes; Mount Rainier, Mount Hood, Three Sisters, and Mount Shasta . U.S. Geological Survey Professional Paper 1365 . 1986 . 2007-03-06.
  5. [Google Earth]
  6. Web site: Whitney Glacier, USGS MOUNT SHASTA (CA) Topo Map. USGS Quad maps. TopoQuest.com. 2008-07-05.
  7. Book: Harris, Stephen L. . Fire Mountains of the West: The Cascade and Mono Lake Volcanoes (3rd ed.) . . 2005 . 109 . 0-87842-511-X .
  8. Web site: Wong. Kathleen. California Glaciers. California Wild. California Academy of Sciences. 2007-01-23 . https://web.archive.org/web/20061006102003/http://www.calacademy.org/calwild/2005fall/stories/glaciers.html . 2006-10-06.
  9. News: Whitney. David. A growing glacier: Mount Shasta bucks global trend, and researchers cite warming phenomena. The Bee. September 4, 2006. 2007-01-23 . https://web.archive.org/web/20070121071019/http://dwb.sacbee.com/content/news/story/14317368p-15234887c.html . 2007-01-21.
  10. Web site: Trabant . D.C. . R.S. March . D.S. Thomas. Hubbard Glacier, Alaska: Growing and Advancing in Spite of Global Climate Change and the 1986 and 2002 Russell Lake Outburst Floods . U.S. Geological Survey Fact Sheet FS-001-03 . 2003 . 2007-03-06.