Disentangling Carbon Concentration Changes Along Pathways of North Atlantic Subtropical Mode Water

North Atlantic Subtropical Mode Water (NASTMW) serves as a major conduit for dissolved carbon to penetrate into the ocean interior by its wintertime outcropping events. Prior research on NASTMW has concentrated on its physical formation and destruction, as well as Lagrangian pathways and timescales...

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Main Authors: Reijnders, Daan, Bakker, Dorothee C. E., Sebille, Erik Van
Format: Other/Unknown Material
Language:unknown
Published: Authorea, Inc. 2024
Subjects:
Online Access:http://dx.doi.org/10.22541/essoar.170365322.22869313/v2
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spelling crwinnower:10.22541/essoar.170365322.22869313/v2 2024-06-02T08:11:17+00:00 Disentangling Carbon Concentration Changes Along Pathways of North Atlantic Subtropical Mode Water Reijnders, Daan Bakker, Dorothee C. E. Sebille, Erik Van 2024 http://dx.doi.org/10.22541/essoar.170365322.22869313/v2 unknown Authorea, Inc. posted-content 2024 crwinnower https://doi.org/10.22541/essoar.170365322.22869313/v2 2024-05-07T14:19:22Z North Atlantic Subtropical Mode Water (NASTMW) serves as a major conduit for dissolved carbon to penetrate into the ocean interior by its wintertime outcropping events. Prior research on NASTMW has concentrated on its physical formation and destruction, as well as Lagrangian pathways and timescales of water into and out of NASTMW. In this study, we examine how dissolved inorganic carbon (DIC) concentrations are modified along Lagrangian pathways of NASTMW on subannual timescales. We introduce Lagrangian parcels into a physical-biogeochemical model and release these parcels annually over two decades. For different pathways into, out of, and within NASTMW, we calculate changes in DIC concentrations along the path (ΔDIC), distinguishing contributions from vertical mixing and biogeochemical processes. While the mean ΔD for parcels that persist within NASTMW in one year is relatively small at +6 µmol/L, this masks underlying dynamics: individual parcels undergo interspersed DIC depletion and enrichment, spanning several timescales and magnitudes. The strongest ΔDIC is during subduction of water parcels (+101 µmol/L in one year), followed by transport out of NASTMW due to increases in density in water parcels (+10 µmol/L). Most DIC enrichment and depletion regimes span timescales of weeks, related to phytoplankton blooms. However, mixing and biogeochemical processes often oppose one another at short timescales, so the largest net DIC changes occur at timescales of more than 30 days. Our new Lagrangian approach complements bulk Eulerian approaches, which average out this underlying complexity, and is relevant to other biogeochemical studies, for example on marine carbon dioxide removal. Other/Unknown Material North Atlantic The Winnower
institution Open Polar
collection The Winnower
op_collection_id crwinnower
language unknown
description North Atlantic Subtropical Mode Water (NASTMW) serves as a major conduit for dissolved carbon to penetrate into the ocean interior by its wintertime outcropping events. Prior research on NASTMW has concentrated on its physical formation and destruction, as well as Lagrangian pathways and timescales of water into and out of NASTMW. In this study, we examine how dissolved inorganic carbon (DIC) concentrations are modified along Lagrangian pathways of NASTMW on subannual timescales. We introduce Lagrangian parcels into a physical-biogeochemical model and release these parcels annually over two decades. For different pathways into, out of, and within NASTMW, we calculate changes in DIC concentrations along the path (ΔDIC), distinguishing contributions from vertical mixing and biogeochemical processes. While the mean ΔD for parcels that persist within NASTMW in one year is relatively small at +6 µmol/L, this masks underlying dynamics: individual parcels undergo interspersed DIC depletion and enrichment, spanning several timescales and magnitudes. The strongest ΔDIC is during subduction of water parcels (+101 µmol/L in one year), followed by transport out of NASTMW due to increases in density in water parcels (+10 µmol/L). Most DIC enrichment and depletion regimes span timescales of weeks, related to phytoplankton blooms. However, mixing and biogeochemical processes often oppose one another at short timescales, so the largest net DIC changes occur at timescales of more than 30 days. Our new Lagrangian approach complements bulk Eulerian approaches, which average out this underlying complexity, and is relevant to other biogeochemical studies, for example on marine carbon dioxide removal.
format Other/Unknown Material
author Reijnders, Daan
Bakker, Dorothee C. E.
Sebille, Erik Van
spellingShingle Reijnders, Daan
Bakker, Dorothee C. E.
Sebille, Erik Van
Disentangling Carbon Concentration Changes Along Pathways of North Atlantic Subtropical Mode Water
author_facet Reijnders, Daan
Bakker, Dorothee C. E.
Sebille, Erik Van
author_sort Reijnders, Daan
title Disentangling Carbon Concentration Changes Along Pathways of North Atlantic Subtropical Mode Water
title_short Disentangling Carbon Concentration Changes Along Pathways of North Atlantic Subtropical Mode Water
title_full Disentangling Carbon Concentration Changes Along Pathways of North Atlantic Subtropical Mode Water
title_fullStr Disentangling Carbon Concentration Changes Along Pathways of North Atlantic Subtropical Mode Water
title_full_unstemmed Disentangling Carbon Concentration Changes Along Pathways of North Atlantic Subtropical Mode Water
title_sort disentangling carbon concentration changes along pathways of north atlantic subtropical mode water
publisher Authorea, Inc.
publishDate 2024
url http://dx.doi.org/10.22541/essoar.170365322.22869313/v2
genre North Atlantic
genre_facet North Atlantic
op_doi https://doi.org/10.22541/essoar.170365322.22869313/v2
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