A Computer Routing of Unsaturated Flow through Snow.

Computer programs for routing the vertical movement of water through snow have been developed. Previously, manual graphical techniques were used, making calculation of the flow and shock front a very time-consuming procedure. The shock front is dependent on surface melt taking place now as well as t...

Full description

Bibliographic Details
Main Authors: Tucker,Walter B , III, Colbeck,Samuel C
Other Authors: COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER N H
Format: Text
Language:English
Published: 1977
Subjects:
Ice
Online Access:http://www.dtic.mil/docs/citations/ADA040121
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA040121
id ftdtic:ADA040121
record_format openpolar
spelling ftdtic:ADA040121 2023-05-15T16:37:44+02:00 A Computer Routing of Unsaturated Flow through Snow. Tucker,Walter B , III Colbeck,Samuel C COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER N H 1977-05 text/html http://www.dtic.mil/docs/citations/ADA040121 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA040121 en eng http://www.dtic.mil/docs/citations/ADA040121 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Hydrology Limnology and Potamology Snow Ice and Permafrost Computer Programming and Software *WATER FLOW *SNOW COMPUTER PROGRAMS MATHEMATICAL MODELS DENSITY PARTICLE SIZE SHOCK WAVES FORECASTING POROSITY SNOW COVER MATHEMATICAL PREDICTION VERTICAL ORIENTATION ERRORS MELTING RUNOFF SINE WAVES WU001 PE61102A Text 1977 ftdtic 2016-02-20T13:16:41Z Computer programs for routing the vertical movement of water through snow have been developed. Previously, manual graphical techniques were used, making calculation of the flow and shock front a very time-consuming procedure. The shock front is dependent on surface melt taking place now as well as the antecedent flow in the snow, usually a function of the nature of the flow for the previous day. One program, designed to accommodate actual surface melt data, has the ability to handle complicated input profiles such as when melt is erratic on a cloudy day, creating such complexities as intersecting shock fronts. Another program, designed for rapid simulation purposes, approximates a simple surface input with a function, in this case a sine wave. This function is easily changed, allowing a variety of conditions to be assessed, although only one shock front is accommodated. Error analysis and some applications of the programs are presented. (Author) Text Ice permafrost Defense Technical Information Center: DTIC Technical Reports database
institution Open Polar
collection Defense Technical Information Center: DTIC Technical Reports database
op_collection_id ftdtic
language English
topic Hydrology
Limnology and Potamology
Snow
Ice and Permafrost
Computer Programming and Software
*WATER FLOW
*SNOW
COMPUTER PROGRAMS
MATHEMATICAL MODELS
DENSITY
PARTICLE SIZE
SHOCK WAVES
FORECASTING
POROSITY
SNOW COVER
MATHEMATICAL PREDICTION
VERTICAL ORIENTATION
ERRORS
MELTING
RUNOFF
SINE WAVES
WU001
PE61102A
spellingShingle Hydrology
Limnology and Potamology
Snow
Ice and Permafrost
Computer Programming and Software
*WATER FLOW
*SNOW
COMPUTER PROGRAMS
MATHEMATICAL MODELS
DENSITY
PARTICLE SIZE
SHOCK WAVES
FORECASTING
POROSITY
SNOW COVER
MATHEMATICAL PREDICTION
VERTICAL ORIENTATION
ERRORS
MELTING
RUNOFF
SINE WAVES
WU001
PE61102A
Tucker,Walter B , III
Colbeck,Samuel C
A Computer Routing of Unsaturated Flow through Snow.
topic_facet Hydrology
Limnology and Potamology
Snow
Ice and Permafrost
Computer Programming and Software
*WATER FLOW
*SNOW
COMPUTER PROGRAMS
MATHEMATICAL MODELS
DENSITY
PARTICLE SIZE
SHOCK WAVES
FORECASTING
POROSITY
SNOW COVER
MATHEMATICAL PREDICTION
VERTICAL ORIENTATION
ERRORS
MELTING
RUNOFF
SINE WAVES
WU001
PE61102A
description Computer programs for routing the vertical movement of water through snow have been developed. Previously, manual graphical techniques were used, making calculation of the flow and shock front a very time-consuming procedure. The shock front is dependent on surface melt taking place now as well as the antecedent flow in the snow, usually a function of the nature of the flow for the previous day. One program, designed to accommodate actual surface melt data, has the ability to handle complicated input profiles such as when melt is erratic on a cloudy day, creating such complexities as intersecting shock fronts. Another program, designed for rapid simulation purposes, approximates a simple surface input with a function, in this case a sine wave. This function is easily changed, allowing a variety of conditions to be assessed, although only one shock front is accommodated. Error analysis and some applications of the programs are presented. (Author)
author2 COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER N H
format Text
author Tucker,Walter B , III
Colbeck,Samuel C
author_facet Tucker,Walter B , III
Colbeck,Samuel C
author_sort Tucker,Walter B , III
title A Computer Routing of Unsaturated Flow through Snow.
title_short A Computer Routing of Unsaturated Flow through Snow.
title_full A Computer Routing of Unsaturated Flow through Snow.
title_fullStr A Computer Routing of Unsaturated Flow through Snow.
title_full_unstemmed A Computer Routing of Unsaturated Flow through Snow.
title_sort computer routing of unsaturated flow through snow.
publishDate 1977
url http://www.dtic.mil/docs/citations/ADA040121
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA040121
genre Ice
permafrost
genre_facet Ice
permafrost
op_source DTIC AND NTIS
op_relation http://www.dtic.mil/docs/citations/ADA040121
op_rights APPROVED FOR PUBLIC RELEASE
_version_ 1766028036716625920