52 Paleoclimate II (Posters)
Monday, 28 July 2003
1:30 PM - 4:30 PM
RESPONSE OF U.S. GLACIERS TO POST-LITTLE-ICE-AGE CLIMATE
Paper number: 52-4
Program: Technical Sessions
Time: 1:30 PM – 4:30 PM
Authors
Abstract
In the WCS (Washington, Oregon, California, Montana, Wyoming, Colorado, Idaho, Utah, and Nevada), every area investigated is characterized by significant glacier retreat, thinning, and/or stagnation, especially at lower elevations. At some locations, glaciers have completely disappeared during the 20th century. In places, retreat that started pre-mid-19th century has continued into the 21st century.
In AK, every glacier ending below ~ 1,500 m in the Wrangell Mountains, Alaska Range, Talkeetna Mountains, Ahklun-Wood River Mountains, Kigluaik Mountains, Brooks Range, Alexander Archipelago, Aleutian Islands, and on Kodiak Island is retreating, thinning, and/or stagnating. In the Coast Mountains, Saint Elias Mountains, Chugach Mountains, Kenai Mountains, and the Aleutian Range, more than 98% of glaciers ending below ~ 1,500 m are also retreating, thinning, and/or stagnating. However, ~ 15 glaciers are currently advancing. Some advancing glaciers have tidewater termini. Many glaciers have disappeared during the 20th century. In places, retreat is resulting in the number of glaciers increasing, but volume and area decreasing. Glaciers at elevations above ~ 1,500 m show little or no change.
AK's two largest glaciers, Bering and Malaspina, are thinning and retreating, losing several cubic kilometers of ice each year to melting and calving. U.S. glaciers are a major contributor of meltwater to global sea level rise, with > 99% coming from AK.