Model results of sensitivity experiments for marine nitrogen cycle in four NetCDF files ...

The marine nitrogen (N) inventory is thought to be stabilized by negative feedback mechanisms that reduce N inventory excursions relative to the more slowly overturning phosphorus inventory. Using a global biogeochemical ocean circulation model we show that negative feedbacks stabilizing the N inven...

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Main Authors: Landolfi, Angela, Dietze, Heiner, Koeve, Wolfgang, Oschlies, Andreas
Format: Dataset
Language:English
Published: PANGAEA 2013
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.833155
https://doi.pangaea.de/10.1594/PANGAEA.833155
id ftdatacite:10.1594/pangaea.833155
record_format openpolar
spelling ftdatacite:10.1594/pangaea.833155 2024-09-15T18:28:13+00:00 Model results of sensitivity experiments for marine nitrogen cycle in four NetCDF files ... Landolfi, Angela Dietze, Heiner Koeve, Wolfgang Oschlies, Andreas 2013 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.833155 https://doi.pangaea.de/10.1594/PANGAEA.833155 en eng PANGAEA https://dx.doi.org/10.5194/bg-10-1351-2013 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 File format File size Uniform resource locator/link to model result file Description modelled Biological Impacts of Ocean Acidification BIOACID dataset Supplementary Dataset Dataset 2013 ftdatacite https://doi.org/10.1594/pangaea.83315510.5194/bg-10-1351-2013 2024-08-01T10:57:37Z The marine nitrogen (N) inventory is thought to be stabilized by negative feedback mechanisms that reduce N inventory excursions relative to the more slowly overturning phosphorus inventory. Using a global biogeochemical ocean circulation model we show that negative feedbacks stabilizing the N inventory cannot persist if a close spatial association of N2 fixation and denitrification occurs. In our idealized model experiments, nitrogen deficient waters, generated by denitrification, stimulate local N2 fixation activity. But, because of stoichiometric constraints, the denitrification of newly fixed nitrogen leads to a net loss of N. This can enhance the N deficit, thereby triggering additional fixation in a vicious cycle, ultimately leading to a runaway N loss. To break this vicious cycle, and allow for stabilizing negative feedbacks to occur, inputs of new N need to be spatially decoupled from denitrification. Our idealized model experiments suggest that factors such as iron limitation or dissolved organic ... : Supplement to: Landolfi, Angela; Dietze, Heiner; Koeve, Wolfgang; Oschlies, Andreas (2013): Overlooked runaway feedback in the marine nitrogen cycle: the vicious cycle. Biogeosciences, 10(3), 1351-1363 ... Dataset Ocean acidification DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic File format
File size
Uniform resource locator/link to model result file
Description
modelled
Biological Impacts of Ocean Acidification BIOACID
spellingShingle File format
File size
Uniform resource locator/link to model result file
Description
modelled
Biological Impacts of Ocean Acidification BIOACID
Landolfi, Angela
Dietze, Heiner
Koeve, Wolfgang
Oschlies, Andreas
Model results of sensitivity experiments for marine nitrogen cycle in four NetCDF files ...
topic_facet File format
File size
Uniform resource locator/link to model result file
Description
modelled
Biological Impacts of Ocean Acidification BIOACID
description The marine nitrogen (N) inventory is thought to be stabilized by negative feedback mechanisms that reduce N inventory excursions relative to the more slowly overturning phosphorus inventory. Using a global biogeochemical ocean circulation model we show that negative feedbacks stabilizing the N inventory cannot persist if a close spatial association of N2 fixation and denitrification occurs. In our idealized model experiments, nitrogen deficient waters, generated by denitrification, stimulate local N2 fixation activity. But, because of stoichiometric constraints, the denitrification of newly fixed nitrogen leads to a net loss of N. This can enhance the N deficit, thereby triggering additional fixation in a vicious cycle, ultimately leading to a runaway N loss. To break this vicious cycle, and allow for stabilizing negative feedbacks to occur, inputs of new N need to be spatially decoupled from denitrification. Our idealized model experiments suggest that factors such as iron limitation or dissolved organic ... : Supplement to: Landolfi, Angela; Dietze, Heiner; Koeve, Wolfgang; Oschlies, Andreas (2013): Overlooked runaway feedback in the marine nitrogen cycle: the vicious cycle. Biogeosciences, 10(3), 1351-1363 ...
format Dataset
author Landolfi, Angela
Dietze, Heiner
Koeve, Wolfgang
Oschlies, Andreas
author_facet Landolfi, Angela
Dietze, Heiner
Koeve, Wolfgang
Oschlies, Andreas
author_sort Landolfi, Angela
title Model results of sensitivity experiments for marine nitrogen cycle in four NetCDF files ...
title_short Model results of sensitivity experiments for marine nitrogen cycle in four NetCDF files ...
title_full Model results of sensitivity experiments for marine nitrogen cycle in four NetCDF files ...
title_fullStr Model results of sensitivity experiments for marine nitrogen cycle in four NetCDF files ...
title_full_unstemmed Model results of sensitivity experiments for marine nitrogen cycle in four NetCDF files ...
title_sort model results of sensitivity experiments for marine nitrogen cycle in four netcdf files ...
publisher PANGAEA
publishDate 2013
url https://dx.doi.org/10.1594/pangaea.833155
https://doi.pangaea.de/10.1594/PANGAEA.833155
genre Ocean acidification
genre_facet Ocean acidification
op_relation https://dx.doi.org/10.5194/bg-10-1351-2013
op_rights Creative Commons Attribution 3.0 Unported
https://creativecommons.org/licenses/by/3.0/legalcode
cc-by-3.0
op_doi https://doi.org/10.1594/pangaea.83315510.5194/bg-10-1351-2013
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