Heat transfer in 3D water and ice basins
Studying heat transfer in 3D water or ice basins involves the solution of Navier Stokes or Stokes systems of PDE, coupled with a scalar equation for thermal energy transport. The method used in this paper is based on a Finite Volume technique where physical quantities and boundary conditions are app...
Published in: | Advanced Computational Methods in Heat Transfer IX |
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Online Access: | http://hdl.handle.net/10281/11844 https://doi.org/10.2495/HT060141 |
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ftunivmilanobic:oai:boa.unimib.it:10281/11844 2024-02-11T09:56:55+01:00 Heat transfer in 3D water and ice basins Ceci, S Fossati, G DE BIASE, LUCIA Sunden, B Brebbia, CA Ceci, S Fossati, G DE BIASE, L 2006 http://hdl.handle.net/10281/11844 https://doi.org/10.2495/HT060141 eng eng WIT Press country:GB info:eu-repo/semantics/altIdentifier/isbn/9781845641764 info:eu-repo/semantics/altIdentifier/wos/WOS:000239953800014 ispartofbook:9th International Conference on Advanced Computational Methods and Experimental Measurements in Heat and Mass Transfer 2006, HT06 9th International Conference on Advanced Computational Methods and Experimental Measurements in Heat and Mass Transfer 2006, HT06 - 5 July 2006 through 7 July 2006 volume:53 firstpage:143 lastpage:152 numberofpages:10 serie:WIT TRANSACTIONS ON ENGINEERING SCIENCES alleditors:Sunden, B; Brebbia, CA http://hdl.handle.net/10281/11844 doi:10.2495/HT060141 info:eu-repo/semantics/altIdentifier/scopus/2-s2.0-36148961624 Fluid dynamic Glacier modelling Glacier temperature Thermal discharges info:eu-repo/semantics/conferenceObject 2006 ftunivmilanobic https://doi.org/10.2495/HT060141 2024-01-23T23:17:54Z Studying heat transfer in 3D water or ice basins involves the solution of Navier Stokes or Stokes systems of PDE, coupled with a scalar equation for thermal energy transport. The method used in this paper is based on a Finite Volume technique where physical quantities and boundary conditions are approximated by means of high order formulae and the time advance is dealt with by a fractional step technique. This paper is mainly concerned with applications, but, with respect to a preceding version of the method, an evaluation of performance of techniques dealing with the turbulent viscosity in water basins is presented and a study of the temperature field in a glacier is included. The method is applied to a thermal discharge in a water basin of lower temperature and to a portion of the Priestley Glacier (Antarctica). The results are very accurate and coherent with the physical theory and with measured data. Conference Object Antarc* Antarctica Priestley Glacier Università degli Studi di Milano-Bicocca: BOA (Bicocca Open Archive) Priestley ENVELOPE(161.883,161.883,-75.183,-75.183) Priestley Glacier ENVELOPE(163.367,163.367,-74.333,-74.333) Advanced Computational Methods in Heat Transfer IX 1 143 152 |
institution |
Open Polar |
collection |
Università degli Studi di Milano-Bicocca: BOA (Bicocca Open Archive) |
op_collection_id |
ftunivmilanobic |
language |
English |
topic |
Fluid dynamic Glacier modelling Glacier temperature Thermal discharges |
spellingShingle |
Fluid dynamic Glacier modelling Glacier temperature Thermal discharges Ceci, S Fossati, G DE BIASE, LUCIA Heat transfer in 3D water and ice basins |
topic_facet |
Fluid dynamic Glacier modelling Glacier temperature Thermal discharges |
description |
Studying heat transfer in 3D water or ice basins involves the solution of Navier Stokes or Stokes systems of PDE, coupled with a scalar equation for thermal energy transport. The method used in this paper is based on a Finite Volume technique where physical quantities and boundary conditions are approximated by means of high order formulae and the time advance is dealt with by a fractional step technique. This paper is mainly concerned with applications, but, with respect to a preceding version of the method, an evaluation of performance of techniques dealing with the turbulent viscosity in water basins is presented and a study of the temperature field in a glacier is included. The method is applied to a thermal discharge in a water basin of lower temperature and to a portion of the Priestley Glacier (Antarctica). The results are very accurate and coherent with the physical theory and with measured data. |
author2 |
Sunden, B Brebbia, CA Ceci, S Fossati, G DE BIASE, L |
format |
Conference Object |
author |
Ceci, S Fossati, G DE BIASE, LUCIA |
author_facet |
Ceci, S Fossati, G DE BIASE, LUCIA |
author_sort |
Ceci, S |
title |
Heat transfer in 3D water and ice basins |
title_short |
Heat transfer in 3D water and ice basins |
title_full |
Heat transfer in 3D water and ice basins |
title_fullStr |
Heat transfer in 3D water and ice basins |
title_full_unstemmed |
Heat transfer in 3D water and ice basins |
title_sort |
heat transfer in 3d water and ice basins |
publisher |
WIT Press |
publishDate |
2006 |
url |
http://hdl.handle.net/10281/11844 https://doi.org/10.2495/HT060141 |
long_lat |
ENVELOPE(161.883,161.883,-75.183,-75.183) ENVELOPE(163.367,163.367,-74.333,-74.333) |
geographic |
Priestley Priestley Glacier |
geographic_facet |
Priestley Priestley Glacier |
genre |
Antarc* Antarctica Priestley Glacier |
genre_facet |
Antarc* Antarctica Priestley Glacier |
op_relation |
info:eu-repo/semantics/altIdentifier/isbn/9781845641764 info:eu-repo/semantics/altIdentifier/wos/WOS:000239953800014 ispartofbook:9th International Conference on Advanced Computational Methods and Experimental Measurements in Heat and Mass Transfer 2006, HT06 9th International Conference on Advanced Computational Methods and Experimental Measurements in Heat and Mass Transfer 2006, HT06 - 5 July 2006 through 7 July 2006 volume:53 firstpage:143 lastpage:152 numberofpages:10 serie:WIT TRANSACTIONS ON ENGINEERING SCIENCES alleditors:Sunden, B; Brebbia, CA http://hdl.handle.net/10281/11844 doi:10.2495/HT060141 info:eu-repo/semantics/altIdentifier/scopus/2-s2.0-36148961624 |
op_doi |
https://doi.org/10.2495/HT060141 |
container_title |
Advanced Computational Methods in Heat Transfer IX |
container_volume |
1 |
container_start_page |
143 |
op_container_end_page |
152 |
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1790606956393660416 |