Meltrate of basal ice shelves at difference inclination
Direct Numerical Simulation (DNS) was used to study the effect of sloping the ice-shelves on the dissolution/melt rate at the ice-ocean interface. The simulations were done on the HPC Raijin at NCI, Canberra over March 2015 to June 2017. Numerical experiments were carried out over a range of slope a...
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Australian Antarctic Data Centre
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Online Access: | https://researchdata.ands.org.au/meltrate-basal-ice-difference-inclination/1330271 https://doi.org/10.4225/15/5b022497c7b72 https://data.aad.gov.au/metadata/records/AAS_4422_Slope_Meltrate http://nla.gov.au/nla.party-617536 |
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ftands:oai:ands.org.au::1330271 2023-05-15T13:47:00+02:00 Meltrate of basal ice shelves at difference inclination GAYEN, BISAKHDATTA (hasPrincipalInvestigator) GAYEN, BISAKHDATTA (processor) MONDAL, MAINAK (hasPrincipalInvestigator) MONDAL, MAINAK (processor) Australian Antarctic Data Centre (publisher) Spatial: northlimit=-60; southlimit=-90; westlimit=-180; eastLimit=180; projection=WGS84 Temporal: From 2015-03-01 to 2017-06-30 https://researchdata.ands.org.au/meltrate-basal-ice-difference-inclination/1330271 https://doi.org/10.4225/15/5b022497c7b72 https://data.aad.gov.au/metadata/records/AAS_4422_Slope_Meltrate http://nla.gov.au/nla.party-617536 unknown Australian Antarctic Data Centre https://researchdata.ands.org.au/meltrate-basal-ice-difference-inclination/1330271 a8bf7864-e193-4317-8938-666298f59740 doi:10.4225/15/5b022497c7b72 AAS_4422_Slope_Meltrate https://data.aad.gov.au/metadata/records/AAS_4422_Slope_Meltrate http://nla.gov.au/nla.party-617536 Australian Antarctic Data Centre climatologyMeteorologyAtmosphere oceans ICE SHEETS EARTH SCIENCE CRYOSPHERE GLACIERS/ICE SHEETS EARTH SCIENCE > CRYOSPHERE > GLACIERS/ICE SHEETS > ICE SHEETS > ICE SHEET MEASUREMENTS SALINITY SEA ICE SNOW/ICE TEMPERATURE SNOW/ICE DIRECT NUMERICAL SIMULATION DNS SLOPE ANGLE MELT RATE Computer > Computer MODELS EARTH SCIENCE SERVICES GEOGRAPHIC REGION > POLAR CONTINENT > ANTARCTICA OCEAN > SOUTHERN OCEAN dataset ftands https://doi.org/10.4225/15/5b022497c7b72 2020-01-05T22:00:03Z Direct Numerical Simulation (DNS) was used to study the effect of sloping the ice-shelves on the dissolution/melt rate at the ice-ocean interface. The simulations were done on the HPC Raijin at NCI, Canberra over March 2015 to June 2017. Numerical experiments were carried out over a range of slope angle (5 degrees – 90 degrees) of the ice-shelves measured from the horizon. Turbulent flow field is simulated over the domain length of 1.8 m, (for slope angle greater than or equal to 50 degrees) and 20 m (for slope angle less than or equal to 20 degrees) respectively; the flow-field is laminar otherwise. A constant ambient temperature 2.3 degrees C and salinity 35 psu is maintained throughout the simulations. The DNS successfully resolved all possible turbulence length scales and relative contributions of diffusive and turbulent heat transfer into the ice wall is measured. Data available: Excel file Meltrate_vs_slopeangle_lam_turb.xlsx contains both simulated laminar and turbulent dissolution/melt rate as a function of slope angle along with their analytical values based on laminar and turbulent scaling theory respectively. Dataset Antarc* Antarctica Ice Sheet Ice Shelves Sea ice Southern Ocean Research Data Australia (Australian National Data Service - ANDS) Southern Ocean ENVELOPE(-180,180,-60,-90) |
institution |
Open Polar |
collection |
Research Data Australia (Australian National Data Service - ANDS) |
op_collection_id |
ftands |
language |
unknown |
topic |
climatologyMeteorologyAtmosphere oceans ICE SHEETS EARTH SCIENCE CRYOSPHERE GLACIERS/ICE SHEETS EARTH SCIENCE > CRYOSPHERE > GLACIERS/ICE SHEETS > ICE SHEETS > ICE SHEET MEASUREMENTS SALINITY SEA ICE SNOW/ICE TEMPERATURE SNOW/ICE DIRECT NUMERICAL SIMULATION DNS SLOPE ANGLE MELT RATE Computer > Computer MODELS EARTH SCIENCE SERVICES GEOGRAPHIC REGION > POLAR CONTINENT > ANTARCTICA OCEAN > SOUTHERN OCEAN |
spellingShingle |
climatologyMeteorologyAtmosphere oceans ICE SHEETS EARTH SCIENCE CRYOSPHERE GLACIERS/ICE SHEETS EARTH SCIENCE > CRYOSPHERE > GLACIERS/ICE SHEETS > ICE SHEETS > ICE SHEET MEASUREMENTS SALINITY SEA ICE SNOW/ICE TEMPERATURE SNOW/ICE DIRECT NUMERICAL SIMULATION DNS SLOPE ANGLE MELT RATE Computer > Computer MODELS EARTH SCIENCE SERVICES GEOGRAPHIC REGION > POLAR CONTINENT > ANTARCTICA OCEAN > SOUTHERN OCEAN Meltrate of basal ice shelves at difference inclination |
topic_facet |
climatologyMeteorologyAtmosphere oceans ICE SHEETS EARTH SCIENCE CRYOSPHERE GLACIERS/ICE SHEETS EARTH SCIENCE > CRYOSPHERE > GLACIERS/ICE SHEETS > ICE SHEETS > ICE SHEET MEASUREMENTS SALINITY SEA ICE SNOW/ICE TEMPERATURE SNOW/ICE DIRECT NUMERICAL SIMULATION DNS SLOPE ANGLE MELT RATE Computer > Computer MODELS EARTH SCIENCE SERVICES GEOGRAPHIC REGION > POLAR CONTINENT > ANTARCTICA OCEAN > SOUTHERN OCEAN |
description |
Direct Numerical Simulation (DNS) was used to study the effect of sloping the ice-shelves on the dissolution/melt rate at the ice-ocean interface. The simulations were done on the HPC Raijin at NCI, Canberra over March 2015 to June 2017. Numerical experiments were carried out over a range of slope angle (5 degrees – 90 degrees) of the ice-shelves measured from the horizon. Turbulent flow field is simulated over the domain length of 1.8 m, (for slope angle greater than or equal to 50 degrees) and 20 m (for slope angle less than or equal to 20 degrees) respectively; the flow-field is laminar otherwise. A constant ambient temperature 2.3 degrees C and salinity 35 psu is maintained throughout the simulations. The DNS successfully resolved all possible turbulence length scales and relative contributions of diffusive and turbulent heat transfer into the ice wall is measured. Data available: Excel file Meltrate_vs_slopeangle_lam_turb.xlsx contains both simulated laminar and turbulent dissolution/melt rate as a function of slope angle along with their analytical values based on laminar and turbulent scaling theory respectively. |
author2 |
GAYEN, BISAKHDATTA (hasPrincipalInvestigator) GAYEN, BISAKHDATTA (processor) MONDAL, MAINAK (hasPrincipalInvestigator) MONDAL, MAINAK (processor) Australian Antarctic Data Centre (publisher) |
format |
Dataset |
title |
Meltrate of basal ice shelves at difference inclination |
title_short |
Meltrate of basal ice shelves at difference inclination |
title_full |
Meltrate of basal ice shelves at difference inclination |
title_fullStr |
Meltrate of basal ice shelves at difference inclination |
title_full_unstemmed |
Meltrate of basal ice shelves at difference inclination |
title_sort |
meltrate of basal ice shelves at difference inclination |
publisher |
Australian Antarctic Data Centre |
url |
https://researchdata.ands.org.au/meltrate-basal-ice-difference-inclination/1330271 https://doi.org/10.4225/15/5b022497c7b72 https://data.aad.gov.au/metadata/records/AAS_4422_Slope_Meltrate http://nla.gov.au/nla.party-617536 |
op_coverage |
Spatial: northlimit=-60; southlimit=-90; westlimit=-180; eastLimit=180; projection=WGS84 Temporal: From 2015-03-01 to 2017-06-30 |
long_lat |
ENVELOPE(-180,180,-60,-90) |
geographic |
Southern Ocean |
geographic_facet |
Southern Ocean |
genre |
Antarc* Antarctica Ice Sheet Ice Shelves Sea ice Southern Ocean |
genre_facet |
Antarc* Antarctica Ice Sheet Ice Shelves Sea ice Southern Ocean |
op_source |
Australian Antarctic Data Centre |
op_relation |
https://researchdata.ands.org.au/meltrate-basal-ice-difference-inclination/1330271 a8bf7864-e193-4317-8938-666298f59740 doi:10.4225/15/5b022497c7b72 AAS_4422_Slope_Meltrate https://data.aad.gov.au/metadata/records/AAS_4422_Slope_Meltrate http://nla.gov.au/nla.party-617536 |
op_doi |
https://doi.org/10.4225/15/5b022497c7b72 |
_version_ |
1766246205945282560 |