An offline implicit solver for simulating prebomb radiocarbon

It takes several thousand years for the deep-ocean concentration of natural radiocarbon to come to equilibrium with surface fluxes, making it computationally too expensive to routinely simulate it with moderate- to high-resolution ocean models. We present an implicit solver for computing prebomb Δ¹⁴C...

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Published in:Ocean Modelling
Other Authors: Bardin, Ann (author), Primeau, François (author), Lindsay, Keith (author)
Format: Article in Journal/Newspaper
Language:English
Published: Elsevier Ltd. 2014
Subjects:
Online Access:http://nldr.library.ucar.edu/repository/collections/OSGC-000-000-020-222
https://doi.org/10.1016/j.ocemod.2013.09.008
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author2 Bardin, Ann (author)
Primeau, François (author)
Lindsay, Keith (author)
collection OpenSky (NCAR/UCAR - National Center for Atmospheric Research/University Corporation for Atmospheric Research)
container_start_page 45
container_title Ocean Modelling
container_volume 73
description It takes several thousand years for the deep-ocean concentration of natural radiocarbon to come to equilibrium with surface fluxes, making it computationally too expensive to routinely simulate it with moderate- to high-resolution ocean models. We present an implicit solver for computing prebomb Δ¹⁴C that requires the equivalent of only a few tens of model years to reach equilibrium. The solver uses a Newton–Krylov algorithm with a preconditioner based on a coarse-grained annually-averaged tracer-transport operator. Coarse-graining provides a general approach for developing preconditioners for models of increasing resolution. We implemented and tested the solver for the ocean component of the Community Earth System Model (CESM) with a nominal horizontal resolution of 1° x 1° and with 60 vertical levels. Simulated Δ¹⁴C values are in good agreement with observations at the surface and in the North Atlantic, but the deep North Pacific simulated values show a substantial bias, with prebomb radiocarbon Δ¹⁴C values translating to ages that are twice the observationally based estimate. This bias is substantially larger than published simulations obtained with coarser resolution models, suggesting that increasing model resolution does not automatically improve the fidelity of the deep ocean ventilation processes. We therefore recommend that natural Δ¹⁴C be used as a deep-ocean ventilation metric for critically evaluating deep ocean circulation.
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spelling ftncar:oai:drupal-site.org:articles_13179 2025-01-16T23:41:38+00:00 An offline implicit solver for simulating prebomb radiocarbon Bardin, Ann (author) Primeau, François (author) Lindsay, Keith (author) 2014-01-01 http://nldr.library.ucar.edu/repository/collections/OSGC-000-000-020-222 https://doi.org/10.1016/j.ocemod.2013.09.008 en eng Elsevier Ltd. Ocean Modelling http://nldr.library.ucar.edu/repository/collections/OSGC-000-000-020-222 doi:10.1016/j.ocemod.2013.09.008 ark:/85065/d7wh2qwg Copyright 2014 Elsevier Implicit solver Prebomb radiocarbon Newton-Krylov Preconditioner Global ocean modeling Text article 2014 ftncar https://doi.org/10.1016/j.ocemod.2013.09.008 2023-08-14T18:38:36Z It takes several thousand years for the deep-ocean concentration of natural radiocarbon to come to equilibrium with surface fluxes, making it computationally too expensive to routinely simulate it with moderate- to high-resolution ocean models. We present an implicit solver for computing prebomb Δ¹⁴C that requires the equivalent of only a few tens of model years to reach equilibrium. The solver uses a Newton–Krylov algorithm with a preconditioner based on a coarse-grained annually-averaged tracer-transport operator. Coarse-graining provides a general approach for developing preconditioners for models of increasing resolution. We implemented and tested the solver for the ocean component of the Community Earth System Model (CESM) with a nominal horizontal resolution of 1° x 1° and with 60 vertical levels. Simulated Δ¹⁴C values are in good agreement with observations at the surface and in the North Atlantic, but the deep North Pacific simulated values show a substantial bias, with prebomb radiocarbon Δ¹⁴C values translating to ages that are twice the observationally based estimate. This bias is substantially larger than published simulations obtained with coarser resolution models, suggesting that increasing model resolution does not automatically improve the fidelity of the deep ocean ventilation processes. We therefore recommend that natural Δ¹⁴C be used as a deep-ocean ventilation metric for critically evaluating deep ocean circulation. Article in Journal/Newspaper North Atlantic OpenSky (NCAR/UCAR - National Center for Atmospheric Research/University Corporation for Atmospheric Research) Ocean Modelling 73 45 58
spellingShingle Implicit solver
Prebomb radiocarbon
Newton-Krylov Preconditioner
Global ocean modeling
An offline implicit solver for simulating prebomb radiocarbon
title An offline implicit solver for simulating prebomb radiocarbon
title_full An offline implicit solver for simulating prebomb radiocarbon
title_fullStr An offline implicit solver for simulating prebomb radiocarbon
title_full_unstemmed An offline implicit solver for simulating prebomb radiocarbon
title_short An offline implicit solver for simulating prebomb radiocarbon
title_sort offline implicit solver for simulating prebomb radiocarbon
topic Implicit solver
Prebomb radiocarbon
Newton-Krylov Preconditioner
Global ocean modeling
topic_facet Implicit solver
Prebomb radiocarbon
Newton-Krylov Preconditioner
Global ocean modeling
url http://nldr.library.ucar.edu/repository/collections/OSGC-000-000-020-222
https://doi.org/10.1016/j.ocemod.2013.09.008