Accelerated Ice Growth in Rivers
Solid ice growth rates due to the presence of frazil slush beneath the ice cover have been shown to be greater than the so-called static growth. The frazil slush reduces the effective heat of ice solidification and the frazil particles freeze into the interstitial water. Numerical schemes are presen...
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ftdtic:ADA071015 2023-05-15T16:36:52+02:00 Accelerated Ice Growth in Rivers Calkins,Darryl J COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER NH 1979-05 text/html http://www.dtic.mil/docs/citations/ADA071015 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA071015 en eng http://www.dtic.mil/docs/citations/ADA071015 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Hydrology Limnology and Potamology Snow Ice and Permafrost *ICE FORMATION *RIVERS HEAT TRANSFER TEMPERATURE ACCELERATION METEOROLOGICAL DATA FREEZING ICE COLD WEATHER TESTS Frazil ice Ice growth LPN-CWIS-31350 Text 1979 ftdtic 2016-02-20T16:28:19Z Solid ice growth rates due to the presence of frazil slush beneath the ice cover have been shown to be greater than the so-called static growth. The frazil slush reduces the effective heat of ice solidification and the frazil particles freeze into the interstitial water. Numerical schemes are presented which clearly show the effect of frazil ice porosity on ice cover growth rates and the numerical model using air temperature as the major input is compared with field data on ice thickness in a small river laden with frazil ice beneath its cover. (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 *ICE FORMATION *RIVERS HEAT TRANSFER TEMPERATURE ACCELERATION METEOROLOGICAL DATA FREEZING ICE COLD WEATHER TESTS Frazil ice Ice growth LPN-CWIS-31350 |
spellingShingle |
Hydrology Limnology and Potamology Snow Ice and Permafrost *ICE FORMATION *RIVERS HEAT TRANSFER TEMPERATURE ACCELERATION METEOROLOGICAL DATA FREEZING ICE COLD WEATHER TESTS Frazil ice Ice growth LPN-CWIS-31350 Calkins,Darryl J Accelerated Ice Growth in Rivers |
topic_facet |
Hydrology Limnology and Potamology Snow Ice and Permafrost *ICE FORMATION *RIVERS HEAT TRANSFER TEMPERATURE ACCELERATION METEOROLOGICAL DATA FREEZING ICE COLD WEATHER TESTS Frazil ice Ice growth LPN-CWIS-31350 |
description |
Solid ice growth rates due to the presence of frazil slush beneath the ice cover have been shown to be greater than the so-called static growth. The frazil slush reduces the effective heat of ice solidification and the frazil particles freeze into the interstitial water. Numerical schemes are presented which clearly show the effect of frazil ice porosity on ice cover growth rates and the numerical model using air temperature as the major input is compared with field data on ice thickness in a small river laden with frazil ice beneath its cover. (Author) |
author2 |
COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER NH |
format |
Text |
author |
Calkins,Darryl J |
author_facet |
Calkins,Darryl J |
author_sort |
Calkins,Darryl J |
title |
Accelerated Ice Growth in Rivers |
title_short |
Accelerated Ice Growth in Rivers |
title_full |
Accelerated Ice Growth in Rivers |
title_fullStr |
Accelerated Ice Growth in Rivers |
title_full_unstemmed |
Accelerated Ice Growth in Rivers |
title_sort |
accelerated ice growth in rivers |
publishDate |
1979 |
url |
http://www.dtic.mil/docs/citations/ADA071015 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA071015 |
genre |
Ice permafrost |
genre_facet |
Ice permafrost |
op_source |
DTIC AND NTIS |
op_relation |
http://www.dtic.mil/docs/citations/ADA071015 |
op_rights |
APPROVED FOR PUBLIC RELEASE |
_version_ |
1766027194004406272 |