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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Bibliographic Details
Main Author: Calkins,Darryl J
Other Authors: COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER NH
Format: Text
Language:English
Published: 1979
Subjects:
ICE
Ice
Online Access:http://www.dtic.mil/docs/citations/ADA071015
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA071015
id ftdtic:ADA071015
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spelling 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