Twentieth Century Glacier Change on Mount Adams, Washington, USA

  title={Twentieth Century Glacier Change on Mount Adams, Washington, USA},
  author={Danielle J. Sitts and Andrew G. Fountain and Matthew James Hoffman},
Abstract Mount Adams is a large glacier-clad stratovolcano located in southern Washington, USA. We examined the area change of the 12 glaciers on the mountain during the 20th century using historical topographic maps and aerial photographs. The total glacier area decreased by 49% (31.5 km2 to 16.2 km2) from 1904 to 2006. The glaciers showed a period of retreat during the first half of the century, followed by either a slowing of retreat or an advance from the 1960s to the 1990s. Subsequently… 
Glacier variability in the conterminous United States during the twentieth century
Glaciers of the conterminous United States have been receding for the past century. Since 1900 the recession has varied from a 24 % loss in area (Mt. Rainier, Washington) to a 66 % loss in the Lewis
A century of glacier change in the Wind River Range, WY
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Abstract Comparison of historic maps and aerial and ground-based photographs for the small cirque glaciers and glacierets of Rocky Mountain National Park in the northern Front Range of Colorado, USA,
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Abstract Terminus fluctuations of five glaciers and the correspondence of these fluctuations to temperature and precipitation patterns were assessed at Oregon's Mount Hood over the period 1901–2001.
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The glaciers of western Canada and the conterminous United States have dominantly retreated since the end of the Little Ice Age (LIA) in the nineteenth century, although average rates of retreat
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Abstract Eliot Glacier is a small (1.6 km2) glacier on Mount Hood, Oregon, USA, and its ablation zone is largely covered with rock debris. We examine the interrelated processes of ablation rates, ice
Spatial and morphological change on Eliot Glacier , Mount Hood , Oregon , USA
Eliot Glacier is a small (1.6 km) glacier on Mount Hood, Oregon, USA, and its ablation zone is largely covered with rock debris. We examine the interrelated processes of ablation rates, ice thickness
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The spatial characteristics for all glaciers in the North Cascades National Park Complex, USA, were estimated in 1958 and again in 1998. The total glacier area in 1958 was 117.3 � 1.1 km 2 ; by 1998
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The effect of temperate glaciers on runoff variations is examined for the North Cascade Mountains of Washington State. The principal influences of glaciers on streamflow are often unexpected
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Working with comprehensive collections of directly‐measured data on the annual mass balance of glaciers other than the two ice sheets, we combine independent analyses to show that there is broad
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  • 2004
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