Dynamical attribution of oceanic prediction uncertainty in the North Atlantic: application to the design of optimal monitoring systems

In this study, the relation between two approaches to assess the ocean predictability on interannual to decadal time scales is investigated. The first pragmatic approach consists of sampling the initial condition uncertainty and assess the predictability through the divergence of this ensemble in ti...

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Published in:Climate Dynamics
Main Authors: Sévellec, Florian, Dijkstra, Henk A., Drijfhout, Sybren S., Germe, Agathe
Format: Article in Journal/Newspaper
Language:English
Published: 2017
Subjects:
Online Access:https://eprints.soton.ac.uk/416292/
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spelling ftsouthampton:oai:eprints.soton.ac.uk:416292 2023-08-27T04:10:43+02:00 Dynamical attribution of oceanic prediction uncertainty in the North Atlantic: application to the design of optimal monitoring systems Sévellec, Florian Dijkstra, Henk A. Drijfhout, Sybren S. Germe, Agathe 2017-11-17 https://eprints.soton.ac.uk/416292/ English eng Sévellec, Florian, Dijkstra, Henk A., Drijfhout, Sybren S. and Germe, Agathe (2017) Dynamical attribution of oceanic prediction uncertainty in the North Atlantic: application to the design of optimal monitoring systems. Climate Dynamics. (doi:10.1007/s00382-017-3969-2 <http://dx.doi.org/10.1007/s00382-017-3969-2>). Article PeerReviewed 2017 ftsouthampton https://doi.org/10.1007/s00382-017-3969-2 2023-08-03T22:22:43Z In this study, the relation between two approaches to assess the ocean predictability on interannual to decadal time scales is investigated. The first pragmatic approach consists of sampling the initial condition uncertainty and assess the predictability through the divergence of this ensemble in time. The second approach is provided by a theoretical framework to determine error growth by estimating optimal linear growing modes. In this paper, it is shown that under the assumption of linearized dynamics and normal distributions of the uncertainty, the exact quantitative spread of ensemble can be determined from the theoretical framework. This spread is at least an order of magnitude less expensive to compute than the approximate solution given by the pragmatic approach. This result is applied to a state-of-the-art Ocean General Circulation Model to assess the predictability in the North Atlantic of four typical oceanic metrics: the strength of the Atlantic Meridional Overturning Circulation (AMOC), the intensity of its heat transport, the two-dimensional spatially-averaged Sea Surface Temperature (SST) over the North Atlantic, and the three-dimensional spatially-averaged temperature in the North Atlantic. For all tested metrics, except for SST Article in Journal/Newspaper North Atlantic University of Southampton: e-Prints Soton Climate Dynamics 51 4 1517 1535
institution Open Polar
collection University of Southampton: e-Prints Soton
op_collection_id ftsouthampton
language English
description In this study, the relation between two approaches to assess the ocean predictability on interannual to decadal time scales is investigated. The first pragmatic approach consists of sampling the initial condition uncertainty and assess the predictability through the divergence of this ensemble in time. The second approach is provided by a theoretical framework to determine error growth by estimating optimal linear growing modes. In this paper, it is shown that under the assumption of linearized dynamics and normal distributions of the uncertainty, the exact quantitative spread of ensemble can be determined from the theoretical framework. This spread is at least an order of magnitude less expensive to compute than the approximate solution given by the pragmatic approach. This result is applied to a state-of-the-art Ocean General Circulation Model to assess the predictability in the North Atlantic of four typical oceanic metrics: the strength of the Atlantic Meridional Overturning Circulation (AMOC), the intensity of its heat transport, the two-dimensional spatially-averaged Sea Surface Temperature (SST) over the North Atlantic, and the three-dimensional spatially-averaged temperature in the North Atlantic. For all tested metrics, except for SST
format Article in Journal/Newspaper
author Sévellec, Florian
Dijkstra, Henk A.
Drijfhout, Sybren S.
Germe, Agathe
spellingShingle Sévellec, Florian
Dijkstra, Henk A.
Drijfhout, Sybren S.
Germe, Agathe
Dynamical attribution of oceanic prediction uncertainty in the North Atlantic: application to the design of optimal monitoring systems
author_facet Sévellec, Florian
Dijkstra, Henk A.
Drijfhout, Sybren S.
Germe, Agathe
author_sort Sévellec, Florian
title Dynamical attribution of oceanic prediction uncertainty in the North Atlantic: application to the design of optimal monitoring systems
title_short Dynamical attribution of oceanic prediction uncertainty in the North Atlantic: application to the design of optimal monitoring systems
title_full Dynamical attribution of oceanic prediction uncertainty in the North Atlantic: application to the design of optimal monitoring systems
title_fullStr Dynamical attribution of oceanic prediction uncertainty in the North Atlantic: application to the design of optimal monitoring systems
title_full_unstemmed Dynamical attribution of oceanic prediction uncertainty in the North Atlantic: application to the design of optimal monitoring systems
title_sort dynamical attribution of oceanic prediction uncertainty in the north atlantic: application to the design of optimal monitoring systems
publishDate 2017
url https://eprints.soton.ac.uk/416292/
genre North Atlantic
genre_facet North Atlantic
op_relation Sévellec, Florian, Dijkstra, Henk A., Drijfhout, Sybren S. and Germe, Agathe (2017) Dynamical attribution of oceanic prediction uncertainty in the North Atlantic: application to the design of optimal monitoring systems. Climate Dynamics. (doi:10.1007/s00382-017-3969-2 <http://dx.doi.org/10.1007/s00382-017-3969-2>).
op_doi https://doi.org/10.1007/s00382-017-3969-2
container_title Climate Dynamics
container_volume 51
container_issue 4
container_start_page 1517
op_container_end_page 1535
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