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  • 1965-1969  (3)
  • 1
    Publication Date: 1965-01-01
    Description: Early photographs of a cirque glacier complex in the Arrigetch Peaks of the south-central Brooks Range date from 1911, and are the second oldest known set of glacier photographs from northern Alaska. Matching photographs and supplementary observations made in 1962 indicate that changes over the past 51 yr. in this area include general glacial recession and thinning, the emergence of pronounced trimlines and partial melting of ice cores beneath recent moraines.Renewed post-hypsithermal glacial activity in the Arrigetch Peaks area attained two maxima in the recent past. The younger moraines lie close to glacier positions shown in the 1911 photographs, contain ice cores which extend practically to their surfaces and were probably formed in the latter part of the nineteenth century. More weathered deposits, underlain by ice cores at relatively greater depths, were formed at some unknown earlier date. The moraines are correlated with the two-substage recent Fan Mountain advance of northern Alaska and may correspond to dated mid-eighteenth century and middle to late nineteenth century advances of alpine glaciers in the north Pacific coastal mountains of North America.
    Print ISSN: 0022-1430
    Electronic ISSN: 1727-5652
    Topics: Geography , Geosciences
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  • 2
    Publication Date: 1965-01-01
    Description: Early photographs of a cirque glacier complex in the Arrigetch Peaks of the south-central Brooks Range date from 1911, and are the second oldest known set of glacier photographs from northern Alaska. Matching photographs and supplementary observations made in 1962 indicate that changes over the past 51 yr. in this area include general glacial recession and thinning, the emergence of pronounced trimlines and partial melting of ice cores beneath recent moraines.Renewed post-hypsithermal glacial activity in the Arrigetch Peaks area attained two maxima in the recent past. The younger moraines lie close to glacier positions shown in the 1911 photographs, contain ice cores which extend practically to their surfaces and were probably formed in the latter part of the nineteenth century. More weathered deposits, underlain by ice cores at relatively greater depths, were formed at some unknown earlier date. The moraines are correlated with the two-substage recent Fan Mountain advance of northern Alaska and may correspond to dated mid-eighteenth century and middle to late nineteenth century advances of alpine glaciers in the north Pacific coastal mountains of North America.
    Print ISSN: 0022-1430
    Electronic ISSN: 1727-5652
    Topics: Geography , Geosciences
    Location Call Number Expected Availability
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  • 3
    Publication Date: 1965-01-01
    Description: Relates recorded temperature data for Alaska to documented trends of annual world mean temperature, which show a warming trend from 1880 to 1940 followed by cooling (graphed). The records of the 20 Alaskan stations are described in detail and their reliability assessed. The state is divided into five regions, and the trends analyzed exhaustively by region, a composite mean being constructed for the state. Distinction is made between trend and fluctuation, utilizing 4 and 8 yr running means and 3 and 5 yr weighted means (8 yr means graphed). Fluctuation extremes at 7 yr intervals until 1948 are identified, with minor fluctuations subsequently. All regions show a pronounced warm maximum around 1940 with the interior region showing an unusually great warming 1910-1935 (approx 3 F). The 8 yr running means for the Alaska composite 1870-1960 (graphed) shows a close relationship to the world temperature trends for the same period, the warm peak occurring in 1941. The limited precipitation and freeze-thaw data available do not appear to correlate directly with temperature trends.
    Print ISSN: 0004-0843
    Topics: Geography , Geosciences
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