Analysis of River Ice Motion Near a Breaking Front
A quantitative theory of dynamic river ice breakup is not yet available. One of the essential components of such a theory is description of the ice motion near the breaking front. In this report we develop an analysis of this motion for a specific case that is consistent with observed data. The anal...
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ftdtic:ADA243431 2023-05-15T16:37:08+02:00 Analysis of River Ice Motion Near a Breaking Front Ferrick, Michael G. Weyrick, Patricia B. Hunnewell, Susan T. COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER NH 1991-10 text/html http://www.dtic.mil/docs/citations/ADA243431 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA243431 en eng http://www.dtic.mil/docs/citations/ADA243431 Approved for public release; distribution is unlimited. DTIC AND NTIS Hydrology Limnology and Potamology Snow Ice and Permafrost *VELOCITY POSITION(LOCATION) DYNAMICS ACCELERATION THEORY MOTION EQUILIBRIUM(GENERAL) TIME SURFACES ICE CONVERGENCE COVERINGS BEHAVIOR RIVERS CONTINUITY HYDRAULICS RADIUS(MEASURE) ICE BREAKUP MEASUREMENT *ICE BREAKUP *ICE *RIVER ICE PE62730A AST42 WU001 BANKS(WATERWAYS) EQUATIONS OF MOTION BREAKING POINT ICE COVER AREA COVERAGE ICE SHEETS CONNECTICUT RIVER Text 1991 ftdtic 2016-02-22T18:13:29Z A quantitative theory of dynamic river ice breakup is not yet available. One of the essential components of such a theory is description of the ice motion near the breaking front. In this report we develop an analysis of this motion for a specific case that is consistent with observed data. The analysis is generalized by allowing the speed of the breaking front to vary, and the parameters of the ice motion that are obtained represent different dynamic breakup behaviors that have been described previously. The results of the analysis include (1) the hydraulic radius associated with the ice cover and the total ice acceleration as functions of time; (2) the equilibrium ice velocity as a function of bank resistance, and the ice velocity as a function of time for several initial and bank resistance conditions; (3) the time-varying bank resistance at the measurement location; and (4) the time of ice motion, ice velocity, ice acceleration, and the convergence of the moving ice with distance from the breaking front. The measure of ice convergence quantifies the loss of surface area by the sheet that is required for ice continuity, and distinguishes the types of dynamic breakup. Text Ice permafrost Defense Technical Information Center: DTIC Technical Reports database |
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Open Polar |
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Defense Technical Information Center: DTIC Technical Reports database |
op_collection_id |
ftdtic |
language |
English |
topic |
Hydrology Limnology and Potamology Snow Ice and Permafrost *VELOCITY POSITION(LOCATION) DYNAMICS ACCELERATION THEORY MOTION EQUILIBRIUM(GENERAL) TIME SURFACES ICE CONVERGENCE COVERINGS BEHAVIOR RIVERS CONTINUITY HYDRAULICS RADIUS(MEASURE) ICE BREAKUP MEASUREMENT *ICE BREAKUP *ICE *RIVER ICE PE62730A AST42 WU001 BANKS(WATERWAYS) EQUATIONS OF MOTION BREAKING POINT ICE COVER AREA COVERAGE ICE SHEETS CONNECTICUT RIVER |
spellingShingle |
Hydrology Limnology and Potamology Snow Ice and Permafrost *VELOCITY POSITION(LOCATION) DYNAMICS ACCELERATION THEORY MOTION EQUILIBRIUM(GENERAL) TIME SURFACES ICE CONVERGENCE COVERINGS BEHAVIOR RIVERS CONTINUITY HYDRAULICS RADIUS(MEASURE) ICE BREAKUP MEASUREMENT *ICE BREAKUP *ICE *RIVER ICE PE62730A AST42 WU001 BANKS(WATERWAYS) EQUATIONS OF MOTION BREAKING POINT ICE COVER AREA COVERAGE ICE SHEETS CONNECTICUT RIVER Ferrick, Michael G. Weyrick, Patricia B. Hunnewell, Susan T. Analysis of River Ice Motion Near a Breaking Front |
topic_facet |
Hydrology Limnology and Potamology Snow Ice and Permafrost *VELOCITY POSITION(LOCATION) DYNAMICS ACCELERATION THEORY MOTION EQUILIBRIUM(GENERAL) TIME SURFACES ICE CONVERGENCE COVERINGS BEHAVIOR RIVERS CONTINUITY HYDRAULICS RADIUS(MEASURE) ICE BREAKUP MEASUREMENT *ICE BREAKUP *ICE *RIVER ICE PE62730A AST42 WU001 BANKS(WATERWAYS) EQUATIONS OF MOTION BREAKING POINT ICE COVER AREA COVERAGE ICE SHEETS CONNECTICUT RIVER |
description |
A quantitative theory of dynamic river ice breakup is not yet available. One of the essential components of such a theory is description of the ice motion near the breaking front. In this report we develop an analysis of this motion for a specific case that is consistent with observed data. The analysis is generalized by allowing the speed of the breaking front to vary, and the parameters of the ice motion that are obtained represent different dynamic breakup behaviors that have been described previously. The results of the analysis include (1) the hydraulic radius associated with the ice cover and the total ice acceleration as functions of time; (2) the equilibrium ice velocity as a function of bank resistance, and the ice velocity as a function of time for several initial and bank resistance conditions; (3) the time-varying bank resistance at the measurement location; and (4) the time of ice motion, ice velocity, ice acceleration, and the convergence of the moving ice with distance from the breaking front. The measure of ice convergence quantifies the loss of surface area by the sheet that is required for ice continuity, and distinguishes the types of dynamic breakup. |
author2 |
COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER NH |
format |
Text |
author |
Ferrick, Michael G. Weyrick, Patricia B. Hunnewell, Susan T. |
author_facet |
Ferrick, Michael G. Weyrick, Patricia B. Hunnewell, Susan T. |
author_sort |
Ferrick, Michael G. |
title |
Analysis of River Ice Motion Near a Breaking Front |
title_short |
Analysis of River Ice Motion Near a Breaking Front |
title_full |
Analysis of River Ice Motion Near a Breaking Front |
title_fullStr |
Analysis of River Ice Motion Near a Breaking Front |
title_full_unstemmed |
Analysis of River Ice Motion Near a Breaking Front |
title_sort |
analysis of river ice motion near a breaking front |
publishDate |
1991 |
url |
http://www.dtic.mil/docs/citations/ADA243431 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA243431 |
genre |
Ice permafrost |
genre_facet |
Ice permafrost |
op_source |
DTIC AND NTIS |
op_relation |
http://www.dtic.mil/docs/citations/ADA243431 |
op_rights |
Approved for public release; distribution is unlimited. |
_version_ |
1766027436302008320 |