World View of Global Warming

The disintegrating face of the Müller Ice Shelf, Lallemand Fjord, Antarctic Peninsula, 67° South, April 2, 1999. This small shelf, fed by glaciers from the Loubet Coast, has been receding recently after growing over a 400-year cooling period. Like other receding ice shelves such as the larger Larsen, it may be a sensitive monitor of rising regional temperatures. The Larsen Ice Shelf lost a 1200 square mile section early in 2002, prompting some glaciologists to be concerned that even the giant Ross Ice Shelf could be at risk.

This mile-long ice cliff of Marr Ice Piedmont, Anvers Island, has receded about 500 meters since the mid 1960s. The cliff's previous position was to the left of the line of ice floating in the harbor and extended to the headland at the extreme upper left. The regional temperature has increased 5° C in winter over the past 50 years. This reduces seasonal icepack, disrupts growth of krill and changes conditions on penguin rookeries.

Geophysicist Tom Osterkamp indicates ground level when he installed this temperature probe pipe near Denali Park, 15 years ago. Alaska permafrost temperature has increased 0.5° to 1.5° C since 1980, when Osterkamp began measuring ground temperature at 30 sites. Many of those sites show thermokarsting like this. Serious effects include forest damage, sinking roads and buildings, eroding tundra riverbanks, changes in tundra vegetation, and increased carbon dioxide and methane emissions from thawed peat.

Just how serious a threat thawing tundra can be is being measured in Northern Sweden. Rising atmospheric temperatures are causing the disappearance of permafrost and its replacement with marshland or open water.  At Stordalen Mire near Abisko National Park, where careful records and aerial photos were available for comparison, the amount of wetland increased more than 50 % at the expense of higher dry land which had been underlain by permafrost.  Study leader Patrick Crill reports this has increased the emission of methane from the mire, a powerful greenhouse gas, by as much as two-thirds over 1970 emissions.  A 2004 study by Torben Christensen and others directly measured hydrocarbon emissions from the Mire, and found that almost all the emissions were methane.  The scientists express concern that methane emissions seem to increase with temperature and could be a positive feedback creating even more atmospheric warming.

Photographer Gary Braasch holding a 1932 photo of Broggi glacier near Huascaran in the Peruvian Andes, while rephotographing this receding glacier in 1999. Glaciers everywhere in the world (with a very few exceptions) have been shrinking throughout the 20th Century, a prime signal of rapid global warming. Loss of tropical glaciers is particularly rapid. This glacier, previously photographed by the Austrian Hans Kinzl, receded about one kilometer in 67 years.

Here is a series of other receding glaciers in "then and now" views (move cursor over old image to see current glacier position).

Glacier Ururashraju, at about 15,000 feet in Cordillera Blanca of Peru. Photographed in 1986 by Peruvian glaciologist Alcides Ames, whose studies and direction allowed Gary Braasch to rephotograph it in 1999. Retreat of about 500 M. Ames studies confirms the very rapid deglaciation of the Cordillera Blanca, which is the most ice-covered mountain range in the tropics.

Grinnell glacier, Glacier National Park, USA, which has receded almost out of sight. Photographed by a park photographer in 1911 and by Gary Braasch in 2000. Estimates by US National Park Service scientist Dan Fagre are that all but a few of the 30 glaciers in this Northern Rocky Mountains park will be gone by mid-century.

Perhaps the most dramatic glacier withdrawal has been in the Alps, where it has occured in full view of residents, tourists and scientists. This is a 1859 etching of the Rhone glacier in the Kanton of Valais, Switzerland, when the ice filled the valley right to the tiny crossroads of Gletsch. In 2001 the glacier was nearly out of sight, 2.5 km distant and 450 M higher. (Ciceri etching courtesy Stefan Wagner, from Uber die Furka [1999, Limburg a/d/ Lahn, Germany].)

1875 photo courtesy H. Slupetzky/University of Salzburg

The Pasterze, Austria's longest glacier, was about 2 kilometers longer in the 19th C. but is now completely out of sight from this overlook on the Grossglockner High Road. The Margaritzen-Strausee, a dammed artificial lake, now is in the place where the glacier terminus was in 1875. Measurements of the Pasterze began in 1889 and it has been pulling back the entire time, in approximate step with regional temperatures that have been increasing. The glacier is now about eight Km long and loses about 15 meters per year. However in 2003 the Pasterze decreased 30 meters in length and 6.5 meters in thickness. [1875 image, photographer unknown, is courtesy H. Slupetzky, from the University of Salzburg archives. Gary Braasch photo made Aug 14, 2004]

Alaska's glaciers are receding at twice the rate previously thought, according to a new study published in the July 19, 2002 Science journal. These two images show Portage Glacier, near Anchorage, Alaska, in about 1950 and in July 2001. The ice has pulled back nearly out of sight.

Portage Glacier 1950 (historic photo from the Lulu Fairbanks Collection, University of Alaska Library, used by permission.)

Portage Glacier 2002

Portage Glacier 1914

Portage Glacier 2004

Glaciers in the Northwest United States have also been shrinking.  Studies by the Climate Impacts Group at University of Washington show regional temperature has been 1.5° F warmer in the 20th century, with rising snow lines, decreasing mountain snowpack, and earlier spring runoff.  These photos of Mt. Hood Oregon comparing late season snow and ice only 18 years apart indicate the problem:  much less late summer ice from which the region gets water for irrigation, drinking, and fish habitat.

Mt. Hood Oregon August 1984

Mt. Hood Oregon late summer 2002

Greenland's huge icecap, second only to Antarctica, is also showing signs of change, although measurements are preliminary. Outflow glaciers like this one on the central east coast, as measured by NASA airborne radar and laser, appear to be thinning and flowing more rapidly. The National Climate Data Center (NOAA) reports that 2002 saw the greatest measured surface melt of Greenland ice in 24 years of satellite records.  Two deep ice cores from there provide a detailed Northern Hemisphere climate record extending beyond the last ice age.

Around the globe, sea level is about 6 inches higher than it was 100 years ago, due primarily to warmer sea water, along with glacier melting, and the rate of rise is increasing. Leading glaciologist Dr. Mark Meier told a scientific meeting in February 2002 that accepted estimates of sea level rise were underestimated, due to the rapid retreat of mountain glaciers. His estimates are this melting could contribute 0.65 feet or more to sea level this century, which would be added to rise from expansion of warming sea water for a total of 1 to 2 feet by 2100. This is enough to inundate low lying areas from Pacific islands, to Bangladesh, to Florida's low-lying coast and Everglades (see next). In Alaska, the native village of Shishmaref, in the photo to the right, is suffering severe effects of sea level rise.