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Columbia Glacier (Alaska)

Glacier in Alaska, United States

Summary

Glacier in Alaska, United States

Field	Value
name	Columbia Glacier
photo	Columbia Glacier (Alaska) by Sentinel-2.jpg
photo_caption	Satellite image, September 2018
type	Tidewater glacier
location	Descending from the Chugach Mountains to Prince William Sound, Alaska
coords
area	1000 km2
length	51 km
thickness	550 m
terminus	Sealevel (Prince William Sound)
status	Retreating
map	Alaska
label_position	top
mapframe	yes
mapframe-zoom	10
mapframe-wikidata	yes

| mapframe-zoom = 10 | mapframe-wikidata = yes NOTOC The Columbia Glacier, a glacier in Prince William Sound on the south coast of the U.S. state of Alaska, is one of the fastest moving glaciers in the world, and has been retreating since the early 1980s. It was named after Columbia University, one of several glaciers in the area named for elite U.S. colleges by the Harriman Alaska Expedition in 1899. The head of the main branch of the glacier originates at the saddle between Mount Witherspoon and Mount Einstein.

The Alaska Marine Highway vessel M/V Columbia is named after the Columbia Glacier.

Size

An illustration of Columbia Glacier in 1910, with the [[District of Columbia]] overlaid for scale comparisons

The glacier twists its way through western Alaska's Chugach Mountains. The bald streak at the bottom of the mountains, called the trimline, shows this glacier has lost 1,300 ft of thickness. It has also retreated 10.5 mi since that measurement was taken.

Retreat

Satellites have observed Columbia Glacier, one of the fastest-changing glaciers in the world withdraw into the Chugach Mountain Range in south-central Alaska.

The glacier's speed of retreat at the terminus reached a maximum of nearly 30 m per day in 2001, when it was discharging icebergs at approximately 7 km3 per year; the glacier has subsequently slowed down, resulting in an increase in retreat rate. The terminus has retreated a total of 16 km at an average rate of approximately 0.6 km per year since 1982. The retreat has been accompanied by nearly 500 m of thinning at the present position of the terminus. In the next few decades it is expected to retreat another 15 km, to a point where the bed of the glacier rises above sea level. Columbia Glacier's retreat should be completed around 2020. Tidewater glacier advance and retreat is not directly forced by climate (adjacent tidewater glaciers may be simultaneously advancing and retreating), but rapid retreat appears to be triggered by climate-forced long-term thinning.

Gallery

Glacier photographed in 1934

File:Alaska - Columbia Glacier - NARA - 23937601.jpg File:Alaska - Columbia Glacier - NARA - 23937603.jpg File:Alaska - Columbia Glacier - NARA - 23937605.jpg File:Alaska - Columbia Glacier - NARA - 23937609.jpg

References

(1 May 2003). "INSTAAR Glaciology Group". [[University of Colorado at Boulder]].
(26 Nov 2012). "Monte Carlo ice flow modeling projects a new stable configuration for Columbia Glacier Alaska, c. 2020". The Cryosphere.

Wikipedia Source

This article was imported from Wikipedia and is available under the Creative Commons Attribution-ShareAlike 4.0 License. Content has been adapted to SurfDoc format. Original contributors can be found on the article history page.

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