Numerical implementation and oceanographic application of the Gibbs potential of ice
The 2004 Gibbs thermodynamic potential function of naturally abundant water ice is based on much more experimental data than its predecessors, is therefore significantly more accurate and reliable, and for the first time describes the entire temperature and pressure range of existence of this ice ph...
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ftcopernicus:oai:publications.copernicus.org:os6848 2023-05-15T18:17:32+02:00 Numerical implementation and oceanographic application of the Gibbs potential of ice Feistel, R. Wagner, W. Tchijov, V. Guder, C. 2018-01-15 application/pdf https://doi.org/10.5194/os-1-29-2005 https://os.copernicus.org/articles/1/29/2005/ eng eng doi:10.5194/os-1-29-2005 https://os.copernicus.org/articles/1/29/2005/ eISSN: 1812-0792 Text 2018 ftcopernicus https://doi.org/10.5194/os-1-29-2005 2020-07-20T16:27:25Z The 2004 Gibbs thermodynamic potential function of naturally abundant water ice is based on much more experimental data than its predecessors, is therefore significantly more accurate and reliable, and for the first time describes the entire temperature and pressure range of existence of this ice phase. It is expressed in the ITS-90 temperature scale and is consistent with the current scientific pure water standard, IAPWS-95, and the 2003 Gibbs potential of seawater. The combination of these formulations provides sublimation pressures, freezing points, and sea ice properties covering the parameter ranges of oceanographic interest. This paper provides source code examples in Visual Basic, Fortran and C++ for the computation of the Gibbs function of ice and its partial derivatives. It reports the most important related thermodynamic equations for ice and sea ice properties. Text Sea ice Copernicus Publications: E-Journals Ocean Science 1 1 29 38 |
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Open Polar |
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Copernicus Publications: E-Journals |
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ftcopernicus |
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English |
description |
The 2004 Gibbs thermodynamic potential function of naturally abundant water ice is based on much more experimental data than its predecessors, is therefore significantly more accurate and reliable, and for the first time describes the entire temperature and pressure range of existence of this ice phase. It is expressed in the ITS-90 temperature scale and is consistent with the current scientific pure water standard, IAPWS-95, and the 2003 Gibbs potential of seawater. The combination of these formulations provides sublimation pressures, freezing points, and sea ice properties covering the parameter ranges of oceanographic interest. This paper provides source code examples in Visual Basic, Fortran and C++ for the computation of the Gibbs function of ice and its partial derivatives. It reports the most important related thermodynamic equations for ice and sea ice properties. |
format |
Text |
author |
Feistel, R. Wagner, W. Tchijov, V. Guder, C. |
spellingShingle |
Feistel, R. Wagner, W. Tchijov, V. Guder, C. Numerical implementation and oceanographic application of the Gibbs potential of ice |
author_facet |
Feistel, R. Wagner, W. Tchijov, V. Guder, C. |
author_sort |
Feistel, R. |
title |
Numerical implementation and oceanographic application of the Gibbs potential of ice |
title_short |
Numerical implementation and oceanographic application of the Gibbs potential of ice |
title_full |
Numerical implementation and oceanographic application of the Gibbs potential of ice |
title_fullStr |
Numerical implementation and oceanographic application of the Gibbs potential of ice |
title_full_unstemmed |
Numerical implementation and oceanographic application of the Gibbs potential of ice |
title_sort |
numerical implementation and oceanographic application of the gibbs potential of ice |
publishDate |
2018 |
url |
https://doi.org/10.5194/os-1-29-2005 https://os.copernicus.org/articles/1/29/2005/ |
genre |
Sea ice |
genre_facet |
Sea ice |
op_source |
eISSN: 1812-0792 |
op_relation |
doi:10.5194/os-1-29-2005 https://os.copernicus.org/articles/1/29/2005/ |
op_doi |
https://doi.org/10.5194/os-1-29-2005 |
container_title |
Ocean Science |
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1 |
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1 |
container_start_page |
29 |
op_container_end_page |
38 |
_version_ |
1766191812931747840 |