Investigating the predictability of North Atlantic sea surface height

Interannual sea surface height (SSH) forecasts are subject to several sources of uncertainty. Methods relying on statistical forecasts have proven useful in assessing predictability and associated uncertainty due to both initial conditions and boundary conditions. In this study, the interannual pred...

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Published in:Climate Dynamics
Main Authors: Fraser, R, Palmer, M, Roberts, C, Wilson, C, Copsey, D, Zanna, L
Format: Article in Journal/Newspaper
Language:unknown
Published: Springer 2019
Subjects:
Online Access:https://doi.org/10.1007/s00382-019-04814-0
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spelling ftuloxford:oai:ora.ox.ac.uk:uuid:7a464c5a-feba-4747-b294-538a3cdb1a4d 2023-05-15T17:29:42+02:00 Investigating the predictability of North Atlantic sea surface height Fraser, R Palmer, M Roberts, C Wilson, C Copsey, D Zanna, L 2019-07-29 https://doi.org/10.1007/s00382-019-04814-0 https://ora.ox.ac.uk/objects/uuid:7a464c5a-feba-4747-b294-538a3cdb1a4d unknown Springer doi:10.1007/s00382-019-04814-0 https://ora.ox.ac.uk/objects/uuid:7a464c5a-feba-4747-b294-538a3cdb1a4d https://doi.org/10.1007/s00382-019-04814-0 info:eu-repo/semantics/openAccess CC Attribution (CC BY) CC-BY Journal article 2019 ftuloxford https://doi.org/10.1007/s00382-019-04814-0 2022-06-28T20:16:07Z Interannual sea surface height (SSH) forecasts are subject to several sources of uncertainty. Methods relying on statistical forecasts have proven useful in assessing predictability and associated uncertainty due to both initial conditions and boundary conditions. In this study, the interannual predictability of SSH dynamics in the North Atlantic is investigated using the output from a 150 year long control simulation based on HadGEM3, a coupled climate model at eddy-permitting resolution. Linear inverse modeling (LIM) is used to create a statistical model for the evolution of monthly-mean SSH anomalies. The forecasts based on the LIM model demonstrate skill on interannanual timescales O (1–2 years). Forecast skill is found to be largest in both the subtropical and subpolar gyres, with decreased skill in the Gulf Stream extension region. The SSH initial conditions involving a tripolar anomaly off Cape Hatteras lead to a maximum growth in SSH about 20 months later. At this time, there is a meridional shift in the 0 m-SSH contour on the order of 0.5∘–1.5∘-latitude, coupled with a change in SSH along the US East Coast. To complement the LIM-based study, interannual SSH predictability is also quantified using the system’s average predictability time (APT). The APT analysis extracted large-scale SSH patterns which displayed predictability on timescales longer than 2 years. These patterns are responsible for changes in SSH on the order of 10 cm along the US East Coast, driven by variations in Ekman velocity. Our results shed light on the timescales of SSH predictability in the North Atlantic. In addition, the diagnosed optimal initial conditions and predictable patterns could improve interannual forecasts of the Gulf Stream’s characteristics and coastal SSH. Article in Journal/Newspaper North Atlantic ORA - Oxford University Research Archive Climate Dynamics 53 3-4 2175 2195
institution Open Polar
collection ORA - Oxford University Research Archive
op_collection_id ftuloxford
language unknown
description Interannual sea surface height (SSH) forecasts are subject to several sources of uncertainty. Methods relying on statistical forecasts have proven useful in assessing predictability and associated uncertainty due to both initial conditions and boundary conditions. In this study, the interannual predictability of SSH dynamics in the North Atlantic is investigated using the output from a 150 year long control simulation based on HadGEM3, a coupled climate model at eddy-permitting resolution. Linear inverse modeling (LIM) is used to create a statistical model for the evolution of monthly-mean SSH anomalies. The forecasts based on the LIM model demonstrate skill on interannanual timescales O (1–2 years). Forecast skill is found to be largest in both the subtropical and subpolar gyres, with decreased skill in the Gulf Stream extension region. The SSH initial conditions involving a tripolar anomaly off Cape Hatteras lead to a maximum growth in SSH about 20 months later. At this time, there is a meridional shift in the 0 m-SSH contour on the order of 0.5∘–1.5∘-latitude, coupled with a change in SSH along the US East Coast. To complement the LIM-based study, interannual SSH predictability is also quantified using the system’s average predictability time (APT). The APT analysis extracted large-scale SSH patterns which displayed predictability on timescales longer than 2 years. These patterns are responsible for changes in SSH on the order of 10 cm along the US East Coast, driven by variations in Ekman velocity. Our results shed light on the timescales of SSH predictability in the North Atlantic. In addition, the diagnosed optimal initial conditions and predictable patterns could improve interannual forecasts of the Gulf Stream’s characteristics and coastal SSH.
format Article in Journal/Newspaper
author Fraser, R
Palmer, M
Roberts, C
Wilson, C
Copsey, D
Zanna, L
spellingShingle Fraser, R
Palmer, M
Roberts, C
Wilson, C
Copsey, D
Zanna, L
Investigating the predictability of North Atlantic sea surface height
author_facet Fraser, R
Palmer, M
Roberts, C
Wilson, C
Copsey, D
Zanna, L
author_sort Fraser, R
title Investigating the predictability of North Atlantic sea surface height
title_short Investigating the predictability of North Atlantic sea surface height
title_full Investigating the predictability of North Atlantic sea surface height
title_fullStr Investigating the predictability of North Atlantic sea surface height
title_full_unstemmed Investigating the predictability of North Atlantic sea surface height
title_sort investigating the predictability of north atlantic sea surface height
publisher Springer
publishDate 2019
url https://doi.org/10.1007/s00382-019-04814-0
https://ora.ox.ac.uk/objects/uuid:7a464c5a-feba-4747-b294-538a3cdb1a4d
genre North Atlantic
genre_facet North Atlantic
op_relation doi:10.1007/s00382-019-04814-0
https://ora.ox.ac.uk/objects/uuid:7a464c5a-feba-4747-b294-538a3cdb1a4d
https://doi.org/10.1007/s00382-019-04814-0
op_rights info:eu-repo/semantics/openAccess
CC Attribution (CC BY)
op_rightsnorm CC-BY
op_doi https://doi.org/10.1007/s00382-019-04814-0
container_title Climate Dynamics
container_volume 53
container_issue 3-4
container_start_page 2175
op_container_end_page 2195
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