Modelling Seasonally Freezing Ground Conditions.

This projects's aim is to model the spatial distribution of snowcover in areas experiencing seasonally frozen ground. SNOWM1, the model that is currently being developed is an attempt to mathematically model and thereby represent, the distribution of snow within a catchment over the snow season...

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Bibliographic Details
Main Authors: Anderson, M G, Sambles, K M
Other Authors: BRISTOL UNIV (ENGLAND)
Format: Text
Language:English
Published: 1987
Subjects:
Ice
Online Access:http://www.dtic.mil/docs/citations/ADA190970
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA190970
id ftdtic:ADA190970
record_format openpolar
spelling ftdtic:ADA190970 2023-05-15T16:37:47+02:00 Modelling Seasonally Freezing Ground Conditions. Anderson, M G Sambles, K M BRISTOL UNIV (ENGLAND) 1987-11 text/html http://www.dtic.mil/docs/citations/ADA190970 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA190970 en eng http://www.dtic.mil/docs/citations/ADA190970 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Soil Mechanics Snow Ice and Permafrost *FREEZING *SOILS AXES DISTRIBUTION ELEVATION GRAPHICS GROUND LEVEL MATHEMATICAL MODELS MODELS ROTATION SEASONS SLOPE SNOW COVER SPATIAL DISTRIBUTION COMPUTERIZED SIMULATION COMPUTER PROGRAMS *Frozen soils SNOWM1 computer program Text 1987 ftdtic 2016-02-19T10:56:29Z This projects's aim is to model the spatial distribution of snowcover in areas experiencing seasonally frozen ground. SNOWM1, the model that is currently being developed is an attempt to mathematically model and thereby represent, the distribution of snow within a catchment over the snow season. Figure 1 is a graphical representation of the snowcover distribution over the snow season, which SNOWM1 will attempt to mathematically reproduce. Figure 1 considers a plane model slope the position and elevation of which are defined by the coordinates X, Y and Z. X and Z are the axes of rotation, for variations of slope angles and azimuths. The evolution in time of a snow profile at a given point (Xy/Yy) on the slope is shown along the T-axis (points 1,2 and 3). Snowprofile variation with elevation is demonstrated for any time, along the Y-axis (points 4,2 and 5). It is this situation, graphically demonstrated by figure 1, that, when applied to a catchment, the model SNOWM1 is being developed. Text Ice permafrost Defense Technical Information Center: DTIC Technical Reports database The ''Y'' ENVELOPE(-112.453,-112.453,57.591,57.591)
institution Open Polar
collection Defense Technical Information Center: DTIC Technical Reports database
op_collection_id ftdtic
language English
topic Soil Mechanics
Snow
Ice and Permafrost
*FREEZING
*SOILS
AXES
DISTRIBUTION
ELEVATION
GRAPHICS
GROUND LEVEL
MATHEMATICAL MODELS
MODELS
ROTATION
SEASONS
SLOPE
SNOW COVER
SPATIAL DISTRIBUTION
COMPUTERIZED SIMULATION
COMPUTER PROGRAMS
*Frozen soils
SNOWM1 computer program
spellingShingle Soil Mechanics
Snow
Ice and Permafrost
*FREEZING
*SOILS
AXES
DISTRIBUTION
ELEVATION
GRAPHICS
GROUND LEVEL
MATHEMATICAL MODELS
MODELS
ROTATION
SEASONS
SLOPE
SNOW COVER
SPATIAL DISTRIBUTION
COMPUTERIZED SIMULATION
COMPUTER PROGRAMS
*Frozen soils
SNOWM1 computer program
Anderson, M G
Sambles, K M
Modelling Seasonally Freezing Ground Conditions.
topic_facet Soil Mechanics
Snow
Ice and Permafrost
*FREEZING
*SOILS
AXES
DISTRIBUTION
ELEVATION
GRAPHICS
GROUND LEVEL
MATHEMATICAL MODELS
MODELS
ROTATION
SEASONS
SLOPE
SNOW COVER
SPATIAL DISTRIBUTION
COMPUTERIZED SIMULATION
COMPUTER PROGRAMS
*Frozen soils
SNOWM1 computer program
description This projects's aim is to model the spatial distribution of snowcover in areas experiencing seasonally frozen ground. SNOWM1, the model that is currently being developed is an attempt to mathematically model and thereby represent, the distribution of snow within a catchment over the snow season. Figure 1 is a graphical representation of the snowcover distribution over the snow season, which SNOWM1 will attempt to mathematically reproduce. Figure 1 considers a plane model slope the position and elevation of which are defined by the coordinates X, Y and Z. X and Z are the axes of rotation, for variations of slope angles and azimuths. The evolution in time of a snow profile at a given point (Xy/Yy) on the slope is shown along the T-axis (points 1,2 and 3). Snowprofile variation with elevation is demonstrated for any time, along the Y-axis (points 4,2 and 5). It is this situation, graphically demonstrated by figure 1, that, when applied to a catchment, the model SNOWM1 is being developed.
author2 BRISTOL UNIV (ENGLAND)
format Text
author Anderson, M G
Sambles, K M
author_facet Anderson, M G
Sambles, K M
author_sort Anderson, M G
title Modelling Seasonally Freezing Ground Conditions.
title_short Modelling Seasonally Freezing Ground Conditions.
title_full Modelling Seasonally Freezing Ground Conditions.
title_fullStr Modelling Seasonally Freezing Ground Conditions.
title_full_unstemmed Modelling Seasonally Freezing Ground Conditions.
title_sort modelling seasonally freezing ground conditions.
publishDate 1987
url http://www.dtic.mil/docs/citations/ADA190970
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA190970
long_lat ENVELOPE(-112.453,-112.453,57.591,57.591)
geographic The ''Y''
geographic_facet The ''Y''
genre Ice
permafrost
genre_facet Ice
permafrost
op_source DTIC AND NTIS
op_relation http://www.dtic.mil/docs/citations/ADA190970
op_rights APPROVED FOR PUBLIC RELEASE
_version_ 1766028083482066944