Climatic Analogs of Fort Greely, Alaska, and Fort Churchill, Canada, in North America PDF Download
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Author: Andrew D. Hastings
Publisher:
ISBN:
Category : Alaska
Languages : en
Pages : 53
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Book Description
Author: Andrew D. Hastings
Publisher:
ISBN:
Category : Alaska
Languages : en
Pages : 94
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Book Description
Author: Andrew D. Hastings
Publisher:
ISBN:
Category : Alaska
Languages : en
Pages : 53
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Book Description
Author: Sigmund J. Falkowski
Publisher:
ISBN:
Category : Alaska
Languages : en
Pages : 86
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Book Description
Author: Quartermaster Research and Engineering Center (U.S.)
Publisher:
ISBN:
Category : Weather
Languages : en
Pages : 28
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Book Description
Author: Walter Beale Blair
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ISBN:
Category : Africa, Central
Languages : en
Pages : 72
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Author: Walter Beale Blair
Publisher:
ISBN:
Category : Africa, Eastern
Languages : en
Pages : 68
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Book Description
Author: Will F. Thompson
Publisher:
ISBN:
Category : Africa, West
Languages : en
Pages : 64
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Author: Will F. Thompson
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Category : Asia, Southeastern
Languages : en
Pages : 68
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Author:
Publisher:
ISBN:
Category : Science
Languages : en
Pages : 638
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Author: Michael A. Bilello
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ISBN:
Category : Fort Greely (Alaska)
Languages : en
Pages : 44
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Book Description
Observations were made at 19 sites in and around the Fort Greely Military Reservation in Alaska during the winter of 1966-67 to obtain data on the depth and physical properties of the snow cover. Snowfall in 1966-67 totaled 245 cm, which was more than 2-1/2 times the seasonal normal. Maximum snow depths of 80 to 100 cm were observed in a major portion of the reservation. Measurements at nine sites showed that the snow density at Fort Greely was generally light; e.g., the average density in the forest did not exceed 0.24 g/cu cm. However, exceptions such as at Jarvis Creek, where the density averaged 0.33 g/cu cm, could be expected. On the average, less snow falls at Fort Greely than at other interior Alaskan locations; but the average density of the snow cover at all interior Alaska sites is quite light. Relationships between snow-cover properties and climate were tested using data collected at Fort Greely. The results substantiated the relationships between (1) snow hardness and snow density measurements and (2) average snow densities with average windspeed and air temperatures. Snow temperature measurements at Fort Greely showed that the snow in the forest was colder than at exposed sites, primarily because the average air temperature within the forest canopy was lower than that in the open area. (Author).
