Research on the Seasonal Snow of the Arctic Slope. Annual Progress Report, January 16, 1988--December 31, 1988 PDF Download
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Category :
Languages : en
Pages : 12
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Book Description
The original objectives of this research included a regional study of snow on the entire Arctic Slope. During the first year the scope was restricted to the R4D area. In the second and third years the primary focus was also on the R4D area, but measurements were made at Prudhoe Bay, Atgasuk and Wainwright to determine the flux of wind-blown snow on a wider scale. Additional broadening of scope was discussed at the San Diego R4D meetings in April 1986 and 1987 and at the extrapolation workshop held at Penn State University in Spring 1987. The broadening of scope has also included detailed studies of chemistry and controls exerted by large-scale advection of air masses on the longwave, thermal IR, and radiation. The latter phenomena are critical in initiating snowmelt.
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Category :
Languages : en
Pages : 12
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Book Description
The original objectives of this research included a regional study of snow on the entire Arctic Slope. During the first year the scope was restricted to the R4D area. In the second and third years the primary focus was also on the R4D area, but measurements were made at Prudhoe Bay, Atgasuk and Wainwright to determine the flux of wind-blown snow on a wider scale. Additional broadening of scope was discussed at the San Diego R4D meetings in April 1986 and 1987 and at the extrapolation workshop held at Penn State University in Spring 1987. The broadening of scope has also included detailed studies of chemistry and controls exerted by large-scale advection of air masses on the longwave, thermal IR, and radiation. The latter phenomena are critical in initiating snowmelt.
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Category : Power resources
Languages : en
Pages : 654
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Book Description
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ISBN:
Category :
Languages : en
Pages : 5
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Book Description
This project deals with the seasonal snow on Alaska's Arctic Slope. Although it is concentrated on snow of the R4D project area, it is important to relate the snow cover of this area with the rest of the Arctic Slope. The goals include determination of the amount of precipitation which comes as snow, the wind transport of this snow and its depositional pattern as influenced by drifting, the physical properties of the snow, the physical processes which operate in it, the proportions of it which go into evaporation, infiltration and runoff, and the biological role of the snow cover. The 1984--1985, 1985--1986 and 1986--1987 seasonal snow was measured to determine its total quantity, its physical structure and its distribution as a function of wind and topography. Observations of meteorological parameters and snowpack characteristics during winter and spring have yielded information on the seasonal evolution of the snow in quantitative terms. A method of determining melt rates over large regions was developed and is being refined, progress was made on a model describing energy flux sources which control snow melting. A strong control is exerted by air mass advection on a broad scale. We are continuing to devote attention to the sources of energy and energy transfer mechanisms which control snow melt. The 1986 snow melt was two weeks later than the 1987 and 1985 meltouts. The delay was caused by advection of cold air from the Arctic Ocean. When it did get underway melting was very rapid and the snow pack disappeared in only half the time taken in 1985.
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Category : Government publications
Languages : en
Pages : 1200
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ISBN:
Category : Science
Languages : en
Pages : 1774
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Book Description
Author:
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ISBN:
Category :
Languages : en
Pages : 17
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Book Description
This project deals with the seasonal snow on Alaska's Arctic Slope. Although it is concentrated on snow of the R40 project area, it is important to relate the snow cover of this area with the rest of the Arctic Slope. The goals include determination Of the amount of precipitation which comes as snow, the wind transport of this snow and its depositional pattern as influenced by drifting, the physical properties of the snow, the physical processes which operate in it, the proportions of it which go into evaporation, infiltration and runoff, and the biological role of the snow cover.
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ISBN:
Category :
Languages : en
Pages : 11
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Book Description
This project deals with the seasonal snow on Alaska's Arctic Slope. Although it is concentrated on snow of the R4D project area, it is important to relate the snow cover of this area with the rest of the Arctic Slope. The goals include determination of the amount of precipitation which comes as snow, the wind transport of this snow and its depositional pattern as influenced by drifting, the physical properties of the snow, the physical processes which operate in it, the proportions of it which go into evaporation, infiltration and runoff, and the biological role of the snow cover.
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ISBN:
Category : Cold regions
Languages : en
Pages : 578
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Book Description
Author:
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ISBN:
Category :
Languages : en
Pages : 19
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Book Description
This project deals with the seasonal snow on Alaska's Arctic Slope. It is concentrated on snow of the R4D project area. However, an important aspect of this study is to relate the snow cover of this area with the rest of the Arctic Slope. The goals include determination of the amount of precipitation which comes as snow, the wind transport of this snow and its depositional pattern as influenced by drifting, the physical properties of the snow, the physical processes which operate in it, the proportions of it which go into evaporation, infiltration and runoff, and the biological role of the snow cover.
Author:
Publisher:
ISBN:
Category :
Languages : en
Pages : 18
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Book Description
This project deals with the seasonal snow on Alaska's Arctic Slope. Although it is concentrated on snow of the R4D project area, it is important to relate the snow cover of this area with the rest of the Arctic Slope. The goals include determination of the amount of precipitation which comes as snow, the wind transport of this snow and its depositional pattern as influenced by drifting, the physical properties of the snow, the physical processes which operate in it, the proportions of it which go into evaporation, infiltration and runoff, and the biological role of the snow cover.
