Dataset

Meltrate of basal ice shelves at difference inclination

Australian Ocean Data Network
GAYEN, BISAKHDATTA ; MONDAL, MAINAK ; Gayen, B. and Mondal, M. ; Australian Antarctic Division ; Australian Antarctic Data Centre
Viewed: [[ro.stat.viewed]] Cited: [[ro.stat.cited]] Accessed: [[ro.stat.accessed]]
ctx_ver=Z39.88-2004&rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Adc&rfr_id=info%3Asid%2FANDS&rft_id=info:doidoi:10.4225/15/5b022497c7b72&rft.title=Meltrate of basal ice shelves at difference inclination&rft.identifier=doi:10.4225/15/5b022497c7b72&rft.publisher=Australian Antarctic Division&rft.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.There are no quality problems with the dataset.&rft.creator=GAYEN, BISAKHDATTA &rft.creator=MONDAL, MAINAK &rft.creator=Gayen, B. and Mondal, M. &rft.creator=Australian Antarctic Division &rft.creator=Australian Antarctic Data Centre &rft.date=2018&rft.coverage=northlimit=-60; southlimit=-90; westlimit=-180; eastLimit=180&rft.coverage=northlimit=-60; southlimit=-90; westlimit=-180; eastLimit=180&rft_rights=These data are publicly available for download from the provided URL.&rft_rights=This data set conforms to the CCBY Attribution License (http://creativecommons.org/licenses/by/4.0/). Please follow instructions listed in the citation reference provided at http://data.aad.gov.au/aadc/metadata/citation.cfm?entry_id=AAS_4422_Slope_Meltrate when using these data.&rft_subject=climatologyMeteorologyAtmosphere&rft_subject=oceans&rft_subject=ICE SHEETS&rft_subject=EARTH SCIENCE&rft_subject=CRYOSPHERE&rft_subject=GLACIERS/ICE SHEETS&rft_subject=EARTH SCIENCE > CRYOSPHERE > GLACIERS/ICE SHEETS > ICE SHEETS > ICE SHEET MEASUREMENTS&rft_subject=SALINITY&rft_subject=SEA ICE&rft_subject=SNOW/ICE TEMPERATURE&rft_subject=SNOW/ICE&rft_subject=DIRECT NUMERICAL SIMULATION&rft_subject=DNS&rft_subject=SLOPE ANGLE&rft_subject=MELT RATE&rft_subject=Computer > Computer&rft_subject=MODELS&rft_subject=AMD/AU&rft_subject=AMD&rft_subject=CEOS&rft_subject=GEOGRAPHIC REGION > POLAR&rft_subject=CONTINENT > ANTARCTICA&rft_subject=OCEAN > SOUTHERN OCEAN&rft.type=dataset&rft.language=English Access the data

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This data set conforms to the CCBY Attribution License (http://creativecommons.org/licenses/by/4.0/). Please follow instructions listed in the citation reference provided at http://data.aad.gov.au/aadc/metadata/citation.cfm?entry_id=AAS_4422_Slope_Meltrate when using these data.

These data are publicly available for download from the provided URL.

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Full 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.

Lineage

There are no quality problems with the dataset.

Issued: 20180521

Data time period: 2015-03-01 to 2017-06-30

Click to explore relationships graph

180,-60 180,-90 0,-90 -180,-90 -180,-60 0,-60 180,-60

0,-75

text: northlimit=-60; southlimit=-90; westlimit=-180; eastLimit=180

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uri : https://data.aad.gov.au/eds/4654/download

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uri : https://data.aad.gov.au/aadc/metadata/citation.cfm?entry_id=AAS_4422_Slope_Meltrate

Citation reference for this metadata record and dataset.

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uri : https://secure3.aad.gov.au/proms/public/projects/report_project_public.cfm?project_no=AAS_4422

Public information for AAS project AAS_4422

Data Set Citation

uri : https://data.aad.gov.au/metadata/records/AAS_4422_Slope_Meltrate

Meltrate of basal ice shelves at difference inclination

Identifiers