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...

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Published in:Journal of Physical Oceanography
Main Authors: Beron-Vera, Francisco Javier, Olascoaga, Maria Josefina, Helfmann, Luzie, Miron, Philippe
Format: Article in Journal/Newspaper
Language:English
Published: 2023
Subjects:
Online Access:https://opus4.kobv.de/opus4-zib/frontdoor/index/index/docId/8762
https://doi.org/10.1175/JPO-D-22-0172.1
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spelling 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
institution Open Polar
collection Publication Server of Zuse Institute Berlin (ZIB)
op_collection_id 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
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