Water isotope variations in the global ocean model MPI-OM
The stable water isotopes H 2 18 O and HDO are incorporated as passive tracers into the oceanic general circulation model MPI-OM, and a control simulation under present-day climate conditions is analyzed in detail. Both δ 18 O and δD distributions at the ocean surface and deep ocean are generally co...
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ftcopernicus:oai:publications.copernicus.org:gmd14356 2023-05-15T15:05:05+02:00 Water isotope variations in the global ocean model MPI-OM Xu, X. Werner, M. Butzin, M. Lohmann, G. 2018-09-27 application/pdf https://doi.org/10.5194/gmd-5-809-2012 https://gmd.copernicus.org/articles/5/809/2012/ eng eng doi:10.5194/gmd-5-809-2012 https://gmd.copernicus.org/articles/5/809/2012/ eISSN: 1991-9603 Text 2018 ftcopernicus https://doi.org/10.5194/gmd-5-809-2012 2020-07-20T16:25:48Z The stable water isotopes H 2 18 O and HDO are incorporated as passive tracers into the oceanic general circulation model MPI-OM, and a control simulation under present-day climate conditions is analyzed in detail. Both δ 18 O and δD distributions at the ocean surface and deep ocean are generally consistent with available observations on the large scale. The modelled δD-δ 18 O relations in surface waters slightly deviates from the slope of the global meteoric water line in most basins, and a much steeper slope is detected in Arctic Oceans. The simulated deuterium excess of ocean surface waters shows small variations between 80° S and 55° N, and a strong decrease north of 55° N. The model is also able to capture the quasi-linear relationship between δ 18 O and salinity S , as well as δD and S , as seen in observational data. Both in the model results and observations, the surface δ− S relations show a steeper slope in extra-tropical regions than in tropical regions, which indicates relatively more addition of isotopically depleted water at high latitudes. Text Arctic Copernicus Publications: E-Journals Arctic Geoscientific Model Development 5 3 809 818 |
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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 stable water isotopes H 2 18 O and HDO are incorporated as passive tracers into the oceanic general circulation model MPI-OM, and a control simulation under present-day climate conditions is analyzed in detail. Both δ 18 O and δD distributions at the ocean surface and deep ocean are generally consistent with available observations on the large scale. The modelled δD-δ 18 O relations in surface waters slightly deviates from the slope of the global meteoric water line in most basins, and a much steeper slope is detected in Arctic Oceans. The simulated deuterium excess of ocean surface waters shows small variations between 80° S and 55° N, and a strong decrease north of 55° N. The model is also able to capture the quasi-linear relationship between δ 18 O and salinity S , as well as δD and S , as seen in observational data. Both in the model results and observations, the surface δ− S relations show a steeper slope in extra-tropical regions than in tropical regions, which indicates relatively more addition of isotopically depleted water at high latitudes. |
format |
Text |
author |
Xu, X. Werner, M. Butzin, M. Lohmann, G. |
spellingShingle |
Xu, X. Werner, M. Butzin, M. Lohmann, G. Water isotope variations in the global ocean model MPI-OM |
author_facet |
Xu, X. Werner, M. Butzin, M. Lohmann, G. |
author_sort |
Xu, X. |
title |
Water isotope variations in the global ocean model MPI-OM |
title_short |
Water isotope variations in the global ocean model MPI-OM |
title_full |
Water isotope variations in the global ocean model MPI-OM |
title_fullStr |
Water isotope variations in the global ocean model MPI-OM |
title_full_unstemmed |
Water isotope variations in the global ocean model MPI-OM |
title_sort |
water isotope variations in the global ocean model mpi-om |
publishDate |
2018 |
url |
https://doi.org/10.5194/gmd-5-809-2012 https://gmd.copernicus.org/articles/5/809/2012/ |
geographic |
Arctic |
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Arctic |
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Arctic |
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Arctic |
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eISSN: 1991-9603 |
op_relation |
doi:10.5194/gmd-5-809-2012 https://gmd.copernicus.org/articles/5/809/2012/ |
op_doi |
https://doi.org/10.5194/gmd-5-809-2012 |
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Geoscientific Model Development |
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