Ice Loads and Ship Response to Ice. A Second Season
A total of 337 events were collected in the Beaufort Sea in summer multiyear ice conditions. Ship impact speed ranged from 0.5 to almost 6 kts. Ice conditions were generally less severe resulting in lower loads than in 1982. Extremes of the data showed a single sub-panel pressure as high as 1041 psi...
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ftdtic:ADA231528 2023-05-15T15:40:14+02:00 Ice Loads and Ship Response to Ice. A Second Season Daley, C. St John, J. W. Brown, R. Meyer, J. Glen, I. ARCTEC INC COLUMBIA MD 1990-08 text/html http://www.dtic.mil/docs/citations/ADA231528 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA231528 en eng http://www.dtic.mil/docs/citations/ADA231528 Approved for public release; distribution is unlimited. DTIC AND NTIS Snow Ice and Permafrost Marine Engineering *VELOCITY SHIPS IMPACT DATA MANAGEMENT VALIDATION BEAUFORT SEA ICE RESPONSE PRESSURE SUMMER FITTING FUNCTIONS(MATHEMATICS) SEASONS MATHEMATICAL MODELS FINITE ELEMENT ANALYSIS *ICE LOADS *ICE BREAKERS *SEA ICE MULTILAYER ICE LOADS(FORCES) Text 1990 ftdtic 2016-02-22T23:20:26Z A total of 337 events were collected in the Beaufort Sea in summer multiyear ice conditions. Ship impact speed ranged from 0.5 to almost 6 kts. Ice conditions were generally less severe resulting in lower loads than in 1982. Extremes of the data showed a single sub-panel pressure as high as 1041 psi (7.2 MPa) and a maximum total panel force of 374 LT (380 MT). This pressure and force are about 65 and 75%, respectively, of those recorded on the previous deployment to the Beaufort Sea in 1982. Conclusions from the study are: (1) Speed effects were not apparent in the single sub-panel pressure data and only weakly evident in the total force data. (2) Total force and pressure data fit a Gumbel probability distribution for the events collected (337 events). Known multiyear data also fit a Gumbel distribution except for the single sub-panel pressure which fit a Frechet distribution, though there is a very small number of events. (3) Loading the panel with known forces, as was performed in 1982 for validation of the finite element model, showed no significant differences in the measured response. Text Beaufort Sea Ice permafrost Sea ice Defense Technical Information Center: DTIC Technical Reports database Psi ENVELOPE(-63.000,-63.000,-64.300,-64.300) |
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Open Polar |
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Defense Technical Information Center: DTIC Technical Reports database |
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ftdtic |
language |
English |
topic |
Snow Ice and Permafrost Marine Engineering *VELOCITY SHIPS IMPACT DATA MANAGEMENT VALIDATION BEAUFORT SEA ICE RESPONSE PRESSURE SUMMER FITTING FUNCTIONS(MATHEMATICS) SEASONS MATHEMATICAL MODELS FINITE ELEMENT ANALYSIS *ICE LOADS *ICE BREAKERS *SEA ICE MULTILAYER ICE LOADS(FORCES) |
spellingShingle |
Snow Ice and Permafrost Marine Engineering *VELOCITY SHIPS IMPACT DATA MANAGEMENT VALIDATION BEAUFORT SEA ICE RESPONSE PRESSURE SUMMER FITTING FUNCTIONS(MATHEMATICS) SEASONS MATHEMATICAL MODELS FINITE ELEMENT ANALYSIS *ICE LOADS *ICE BREAKERS *SEA ICE MULTILAYER ICE LOADS(FORCES) Daley, C. St John, J. W. Brown, R. Meyer, J. Glen, I. Ice Loads and Ship Response to Ice. A Second Season |
topic_facet |
Snow Ice and Permafrost Marine Engineering *VELOCITY SHIPS IMPACT DATA MANAGEMENT VALIDATION BEAUFORT SEA ICE RESPONSE PRESSURE SUMMER FITTING FUNCTIONS(MATHEMATICS) SEASONS MATHEMATICAL MODELS FINITE ELEMENT ANALYSIS *ICE LOADS *ICE BREAKERS *SEA ICE MULTILAYER ICE LOADS(FORCES) |
description |
A total of 337 events were collected in the Beaufort Sea in summer multiyear ice conditions. Ship impact speed ranged from 0.5 to almost 6 kts. Ice conditions were generally less severe resulting in lower loads than in 1982. Extremes of the data showed a single sub-panel pressure as high as 1041 psi (7.2 MPa) and a maximum total panel force of 374 LT (380 MT). This pressure and force are about 65 and 75%, respectively, of those recorded on the previous deployment to the Beaufort Sea in 1982. Conclusions from the study are: (1) Speed effects were not apparent in the single sub-panel pressure data and only weakly evident in the total force data. (2) Total force and pressure data fit a Gumbel probability distribution for the events collected (337 events). Known multiyear data also fit a Gumbel distribution except for the single sub-panel pressure which fit a Frechet distribution, though there is a very small number of events. (3) Loading the panel with known forces, as was performed in 1982 for validation of the finite element model, showed no significant differences in the measured response. |
author2 |
ARCTEC INC COLUMBIA MD |
format |
Text |
author |
Daley, C. St John, J. W. Brown, R. Meyer, J. Glen, I. |
author_facet |
Daley, C. St John, J. W. Brown, R. Meyer, J. Glen, I. |
author_sort |
Daley, C. |
title |
Ice Loads and Ship Response to Ice. A Second Season |
title_short |
Ice Loads and Ship Response to Ice. A Second Season |
title_full |
Ice Loads and Ship Response to Ice. A Second Season |
title_fullStr |
Ice Loads and Ship Response to Ice. A Second Season |
title_full_unstemmed |
Ice Loads and Ship Response to Ice. A Second Season |
title_sort |
ice loads and ship response to ice. a second season |
publishDate |
1990 |
url |
http://www.dtic.mil/docs/citations/ADA231528 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA231528 |
long_lat |
ENVELOPE(-63.000,-63.000,-64.300,-64.300) |
geographic |
Psi |
geographic_facet |
Psi |
genre |
Beaufort Sea Ice permafrost Sea ice |
genre_facet |
Beaufort Sea Ice permafrost Sea ice |
op_source |
DTIC AND NTIS |
op_relation |
http://www.dtic.mil/docs/citations/ADA231528 |
op_rights |
Approved for public release; distribution is unlimited. |
_version_ |
1766372394566418432 |