Abstract
Abstract
The Coleman Glacier on Mt. Baker in the State of Washington began to advance about 1949 after a long period of rapid retreat. Since that year the terminus has advanced continuously a total of about 300 m. and considerable thickening of the entire glacier has occurred. The continued advance of the Coleman Glacier and other evidence are interpreted as manifestations of a trend during the last decade towards a slightly cooler and moist climate in the north-west of the United States.
Publisher
Cambridge University Press (CUP)
Cited by
8 articles.
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1. North Cascade Range, Washington USA;Recent Climate Change Impacts on Mountain Glaciers;2016-11-04
2. Individual Glacier Behavior;Climate Driven Retreat of Mount Baker Glaciers and Changing Water Resources;2015
3. Terminus Response to Climate Change;Climate Driven Retreat of Mount Baker Glaciers and Changing Water Resources;2015
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5. FOREST GROWTH AND GLACIAL CHRONOLOGY IN EASTERN BRITISH COLUMBIA, AND THEIR RELATION TO RECENT CLIMATIC TRENDS;Canadian Journal of Botany;1963-08-01