Sampling-Dependent Transition Paths of Iceland-Scotland Overflow Water
In this note, we apply Transition Path Theory (TPT) from Markov chains to shed light on the problem of Iceland-Scotland Overflow Water (ISOW) equatorward export. A recent analysis of observed trajectories of submerged floats demanded revision of the traditional abyssal circulation theory, which post...
Published in: | Journal of Physical Oceanography |
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ftziberlin:oai:kobv.de-opus4-zib:8762 2023-12-10T09:49:55+01:00 Sampling-Dependent Transition Paths of Iceland-Scotland Overflow Water Beron-Vera, Francisco Javier Olascoaga, Maria Josefina Helfmann, Luzie Miron, Philippe 2023-01-20 https://opus4.kobv.de/opus4-zib/frontdoor/index/index/docId/8762 https://doi.org/10.1175/JPO-D-22-0172.1 eng eng https://opus4.kobv.de/opus4-zib/frontdoor/index/index/docId/8762 https://doi.org/10.1175/JPO-D-22-0172.1 info:eu-repo/semantics/closedAccess article doc-type:article 2023 ftziberlin https://doi.org/10.1175/JPO-D-22-0172.1 2023-11-12T23:59:21Z In this note, we apply Transition Path Theory (TPT) from Markov chains to shed light on the problem of Iceland-Scotland Overflow Water (ISOW) equatorward export. A recent analysis of observed trajectories of submerged floats demanded revision of the traditional abyssal circulation theory, which postulates that ISOW should steadily flow along a deep boundary current (DBC) around the subpolar North Atlantic prior to exiting it. The TPT analyses carried out here allow to focus the attention on the portions of flow from the origin of ISOW to the region where ISOW exits the subpolar North Atlantic and suggest that insufficient sampling may be biasing the aforementioned demand. The analyses, appropriately adapted to represent a continuous input of ISOW, are carried out on three time-homogeneous Markov chains modeling the ISOW flow. One is constructed using a high number of simulated trajectories homogeneously covering the flow domain. The other two use much fewer trajectories which heterogeneously cover the domain. The trajectories in the latter two chains are observed trajectories or simulated trajectories subsampled at the observed frequency. While the densely sampled chain supports a well-defined DBC, the more heterogeneously sampled chains do not, irrespective of whether observed or simulated trajectories are used. Studying the sampling sensitivity of the Markov chains, we can give recommendations for enlarging the existing float dataset to improve the significance of conclusions about time-asymptotic aspects of the ISOW circulation. Article in Journal/Newspaper Iceland North Atlantic Publication Server of Zuse Institute Berlin (ZIB) Journal of Physical Oceanography |
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Open Polar |
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Publication Server of Zuse Institute Berlin (ZIB) |
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ftziberlin |
language |
English |
description |
In this note, we apply Transition Path Theory (TPT) from Markov chains to shed light on the problem of Iceland-Scotland Overflow Water (ISOW) equatorward export. A recent analysis of observed trajectories of submerged floats demanded revision of the traditional abyssal circulation theory, which postulates that ISOW should steadily flow along a deep boundary current (DBC) around the subpolar North Atlantic prior to exiting it. The TPT analyses carried out here allow to focus the attention on the portions of flow from the origin of ISOW to the region where ISOW exits the subpolar North Atlantic and suggest that insufficient sampling may be biasing the aforementioned demand. The analyses, appropriately adapted to represent a continuous input of ISOW, are carried out on three time-homogeneous Markov chains modeling the ISOW flow. One is constructed using a high number of simulated trajectories homogeneously covering the flow domain. The other two use much fewer trajectories which heterogeneously cover the domain. The trajectories in the latter two chains are observed trajectories or simulated trajectories subsampled at the observed frequency. While the densely sampled chain supports a well-defined DBC, the more heterogeneously sampled chains do not, irrespective of whether observed or simulated trajectories are used. Studying the sampling sensitivity of the Markov chains, we can give recommendations for enlarging the existing float dataset to improve the significance of conclusions about time-asymptotic aspects of the ISOW circulation. |
format |
Article in Journal/Newspaper |
author |
Beron-Vera, Francisco Javier Olascoaga, Maria Josefina Helfmann, Luzie Miron, Philippe |
spellingShingle |
Beron-Vera, Francisco Javier Olascoaga, Maria Josefina Helfmann, Luzie Miron, Philippe Sampling-Dependent Transition Paths of Iceland-Scotland Overflow Water |
author_facet |
Beron-Vera, Francisco Javier Olascoaga, Maria Josefina Helfmann, Luzie Miron, Philippe |
author_sort |
Beron-Vera, Francisco Javier |
title |
Sampling-Dependent Transition Paths of Iceland-Scotland Overflow Water |
title_short |
Sampling-Dependent Transition Paths of Iceland-Scotland Overflow Water |
title_full |
Sampling-Dependent Transition Paths of Iceland-Scotland Overflow Water |
title_fullStr |
Sampling-Dependent Transition Paths of Iceland-Scotland Overflow Water |
title_full_unstemmed |
Sampling-Dependent Transition Paths of Iceland-Scotland Overflow Water |
title_sort |
sampling-dependent transition paths of iceland-scotland overflow water |
publishDate |
2023 |
url |
https://opus4.kobv.de/opus4-zib/frontdoor/index/index/docId/8762 https://doi.org/10.1175/JPO-D-22-0172.1 |
genre |
Iceland North Atlantic |
genre_facet |
Iceland North Atlantic |
op_relation |
https://opus4.kobv.de/opus4-zib/frontdoor/index/index/docId/8762 https://doi.org/10.1175/JPO-D-22-0172.1 |
op_rights |
info:eu-repo/semantics/closedAccess |
op_doi |
https://doi.org/10.1175/JPO-D-22-0172.1 |
container_title |
Journal of Physical Oceanography |
_version_ |
1784894667920244736 |