A dynamics-weighted principal components analysis of dominant atmospheric drivers of ocean variability with an application to the North Atlantic Subpolar Gyre

This paper describes a framework for identifying dominant atmospheric drivers of ocean variability. The method combines statistics of atmosphere-ocean fluxes with physics from an ocean general circulation model to derive atmospheric patterns optimized to excite variability in a specified ocean quant...

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Published in:Journal of Climate
Other Authors: Amrhein, Daniel E. (author), Stephenson, Dafydd (author), Thompson, LuAnne (author)
Format: Article in Journal/Newspaper
Language:English
Published: 2024
Subjects:
Online Access:https://doi.org/10.1175/JCLI-D-23-0197.1
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spelling ftncar:oai:drupal-site.org:articles_27117 2024-05-19T07:44:41+00:00 A dynamics-weighted principal components analysis of dominant atmospheric drivers of ocean variability with an application to the North Atlantic Subpolar Gyre Amrhein, Daniel E. (author) Stephenson, Dafydd (author) Thompson, LuAnne (author) 2024-04-15 https://doi.org/10.1175/JCLI-D-23-0197.1 en eng Journal of Climate--0894-8755--1520-0442 articles:27117 doi:10.1175/JCLI-D-23-0197.1 ark:/85065/d7028wpk Copyright 2024 American Meteorological Society (AMS). article Text 2024 ftncar https://doi.org/10.1175/JCLI-D-23-0197.1 2024-05-02T00:23:33Z This paper describes a framework for identifying dominant atmospheric drivers of ocean variability. The method combines statistics of atmosphere-ocean fluxes with physics from an ocean general circulation model to derive atmospheric patterns optimized to excite variability in a specified ocean quantity of interest. We first derive the method as a weighted principal components analysis and illustrate its capabilities in a toy problem. Next, we apply our analysis to the adjoint of the MITgcm and atmosphere-ocean fluxes from the ECCOv4-r4 state estimate. An unweighted principal components analysis reveals that North Atlantic heat and momentum fluxes in ECCOv4-r4 have a range of spatiotemporal patterns. By contrast, dynamics-weighted principal components analysis collapses the space of these patterns onto a small subset-principally associated with the North Atlantic Oscillation-that dominates interannual SPG HC variance. By perturbing the ECCOv4-r4 state estimate, we illustrate the pathways along which variability propagates from the atmosphere to the ocean in a nonlinear ocean model. This technique is applicable across a range of problems across Earth system components, including in the absence of a model adjoint. 1852977 80NSSC20K0787 Article in Journal/Newspaper North Atlantic North Atlantic oscillation OpenSky (NCAR/UCAR - National Center for Atmospheric Research/University Corporation for Atmospheric Research) Journal of Climate 37 8 2673 2693
institution Open Polar
collection OpenSky (NCAR/UCAR - National Center for Atmospheric Research/University Corporation for Atmospheric Research)
op_collection_id ftncar
language English
description This paper describes a framework for identifying dominant atmospheric drivers of ocean variability. The method combines statistics of atmosphere-ocean fluxes with physics from an ocean general circulation model to derive atmospheric patterns optimized to excite variability in a specified ocean quantity of interest. We first derive the method as a weighted principal components analysis and illustrate its capabilities in a toy problem. Next, we apply our analysis to the adjoint of the MITgcm and atmosphere-ocean fluxes from the ECCOv4-r4 state estimate. An unweighted principal components analysis reveals that North Atlantic heat and momentum fluxes in ECCOv4-r4 have a range of spatiotemporal patterns. By contrast, dynamics-weighted principal components analysis collapses the space of these patterns onto a small subset-principally associated with the North Atlantic Oscillation-that dominates interannual SPG HC variance. By perturbing the ECCOv4-r4 state estimate, we illustrate the pathways along which variability propagates from the atmosphere to the ocean in a nonlinear ocean model. This technique is applicable across a range of problems across Earth system components, including in the absence of a model adjoint. 1852977 80NSSC20K0787
author2 Amrhein, Daniel E. (author)
Stephenson, Dafydd (author)
Thompson, LuAnne (author)
format Article in Journal/Newspaper
title A dynamics-weighted principal components analysis of dominant atmospheric drivers of ocean variability with an application to the North Atlantic Subpolar Gyre
spellingShingle A dynamics-weighted principal components analysis of dominant atmospheric drivers of ocean variability with an application to the North Atlantic Subpolar Gyre
title_short A dynamics-weighted principal components analysis of dominant atmospheric drivers of ocean variability with an application to the North Atlantic Subpolar Gyre
title_full A dynamics-weighted principal components analysis of dominant atmospheric drivers of ocean variability with an application to the North Atlantic Subpolar Gyre
title_fullStr A dynamics-weighted principal components analysis of dominant atmospheric drivers of ocean variability with an application to the North Atlantic Subpolar Gyre
title_full_unstemmed A dynamics-weighted principal components analysis of dominant atmospheric drivers of ocean variability with an application to the North Atlantic Subpolar Gyre
title_sort dynamics-weighted principal components analysis of dominant atmospheric drivers of ocean variability with an application to the north atlantic subpolar gyre
publishDate 2024
url https://doi.org/10.1175/JCLI-D-23-0197.1
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
op_relation Journal of Climate--0894-8755--1520-0442
articles:27117
doi:10.1175/JCLI-D-23-0197.1
ark:/85065/d7028wpk
op_rights Copyright 2024 American Meteorological Society (AMS).
op_doi https://doi.org/10.1175/JCLI-D-23-0197.1
container_title Journal of Climate
container_volume 37
container_issue 8
container_start_page 2673
op_container_end_page 2693
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