Glaciers of New Zealand

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Franz Josef Glacier. Franz Josef glacier.JPG
Franz Josef Glacier.

New Zealand contains many glaciers, mostly located near the Main Divide of the Southern Alps in the South Island. They are classed as mid-latitude mountain glaciers. There are eight small glaciers in the North Island on Mount Ruapehu.

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An inventory of South Island glaciers compiled in the 1980s indicated there were about 3,155 glaciers with an area of at least one hectare (2.5 acres). [1] Approximately one sixth of these glaciers covered more than 10 hectares. These include:

New Zealand's territorial claim in Antarctica, the Ross Dependency, also contains many glaciers.

Retreat of glaciers

The Mueller, Hooker and Tasman glaciers have continued to retreat rapidly in recent years. Notice the larger terminal lakes, the retreat of the white ice (ice free of moraine cover), and the higher moraine walls due to ice thinning. Photo. Tasman Glacier.gif
The Mueller, Hooker and Tasman glaciers have continued to retreat rapidly in recent years. Notice the larger terminal lakes, the retreat of the white ice (ice free of moraine cover), and the higher moraine walls due to ice thinning. Photo.

New Zealand glaciers have been retreating since 1890, with an acceleration of this retreat since 1920. Most of the glaciers have thinned measurably and have reduced in size, and the snow accumulation zones have risen in elevation during the 20th century. In the period 1971–75, Ivory Glacier receded 30 m (98 ft) from the glacial terminus, and about 26% of the surface area of the glacier was lost over the same period.

Since 1980 numerous small glacial lakes were created behind the new terminal moraines of several of these glaciers. Glaciers such as Classen, Godley and Douglas now all have new glacial lakes below their terminal locations due to the glacial retreat over the past 20 years. Satellite imagery indicates that these lakes are continuing to expand. There has been significant and ongoing losses of ice volumes on the largest glaciers: the Tasman, Ivory, Classen, Mueller, Maud, Hooker, Grey, Godley, Ramsay, Murchison, Therma, Volta and Douglas Glaciers. The retreat of these glaciers has been marked by expanding proglacial lakes and terminus region thinning. The loss in volume from 1975–2005 is 11 percent of the total. [2]

Several glaciers, notably the much-visited Fox and Franz Josef Glaciers on the West Coast, have periodically advanced, especially during the 1990s, but the scale of these advances is small when compared to 20th-century retreat. Both glaciers are currently more than 2.5 km (1.6 mi) shorter than a century ago. These large, rapidly flowing glaciers situated on steep slopes have been very reactive to small mass-balance changes. A few years of conditions favorable to glacier advance, such as more westerly winds and a resulting increase in snowfall, are rapidly echoed in a corresponding advance, followed by equally rapid retreat when those favorable conditions end. [3] Hence glacier advance in a few locations is regarded as due to transient local weather conditions which brought more precipitation and cloudier, cooler summers since 2002.

See also

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<span class="mw-page-title-main">Hooker Lake</span> Proglacial lake in Mount Cook National Park, South Island

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<span class="mw-page-title-main">Dart Glacier</span>

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<span class="mw-page-title-main">Geography of the South Island</span> Overview of the Geography of South Island

The South Island, with an area of 150,437 km2 (58,084 sq mi), is the largest landmass of New Zealand; it contains about one-quarter of the New Zealand population and is the world's 12th-largest island. It is divided along its length by the Southern Alps, the highest peak of which is Aoraki / Mount Cook at 3,724 metres (12,218 ft), making it 9th-highest island, with the high Kaikōura Ranges to the northeast. There are eighteen peaks of more than 3,000 metres (9,800 ft) in the South Island. The east side of the island is home to the Canterbury Plains while the West Coast is famous for its rough coastlines such as Fiordland, a very high proportion of native bush, and Fox and Franz Josef Glaciers. The dramatic landscape of the South Island has made it a popular location for the production of several films, including The Lord of the Rings trilogy and The Chronicles of Narnia: The Lion, the Witch and the Wardrobe. It lies at similar latitudes to Tasmania, and parts of Patagonia in South America.

References

  1. Chinn, Trevor J.H., (1988), Glaciers of New Zealand, in Satellite image atlas of glaciers of the world, U.S. Geological Survey professional paper; 1386, ISBN   0-607-71457-3.
  2. Salinger, Jim and Andrew Willsman (February 2007). "Annual Glacier Volumes in New Zealand 1995–2005". NIWA Client Report: AKL2007-014. Statistics New Zealand. Archived from the original (PDF) on 9 June 2011. Retrieved 5 November 2009.
  3. U.S. Geological Survey, United States Department of the Interior (5 April 2000). "Glaciers of New Zealand".