Seafloor organic carbon flux output from the NEMO-MEDUSA model ...
This output was produced by a simulation using a coupled ocean physics and marine biogeochemistry model. The physical ocean submodel was the Nucleus for European Modeling of the Ocean (NEMO) physical ocean model (Madec, 2014), run here in a global 1/12-degree resolution configuration (ORCA0083). The...
Main Author: | |
---|---|
Format: | Dataset |
Language: | English |
Published: |
Zenodo
2022
|
Subjects: | |
Online Access: | https://dx.doi.org/10.5281/zenodo.6513616 https://zenodo.org/record/6513616 |
id |
ftdatacite:10.5281/zenodo.6513616 |
---|---|
record_format |
openpolar |
spelling |
ftdatacite:10.5281/zenodo.6513616 2023-06-11T04:16:35+02:00 Seafloor organic carbon flux output from the NEMO-MEDUSA model ... Yool, Andrew 2022 https://dx.doi.org/10.5281/zenodo.6513616 https://zenodo.org/record/6513616 en eng Zenodo https://dx.doi.org/10.5281/zenodo.6513615 Open Access Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 info:eu-repo/semantics/openAccess marine biogeochemistry marine biogeochemistry ocean model MEDUSA NEMO hindcast simulation seafloor organic carbon flux Dataset dataset 2022 ftdatacite https://doi.org/10.5281/zenodo.651361610.5281/zenodo.6513615 2023-05-02T11:03:53Z This output was produced by a simulation using a coupled ocean physics and marine biogeochemistry model. The physical ocean submodel was the Nucleus for European Modeling of the Ocean (NEMO) physical ocean model (Madec, 2014), run here in a global 1/12-degree resolution configuration (ORCA0083). The marine biogeochemistry submodel was the Model of Ecosystem Dynamics, nutrient Utilisation, Sequestration and Acidification (MEDUSA-2), an intermediate-complexity plankton ecosystem model (Yool et al., 2013). The horizontal resolution of this configuration of NEMO has non-uniform grid cells ranging 2 to 9 km in size (mean 7.5 km), with 75 vertical depth levels (31 levels between the surface and 200 m depth). Sea-ice is represented in the model by the Louvian‐la‐Neuve Ice Model (LIM2) (Fichefet, & Maqueda, M. a. M., 1997; Goosse & Fichefet, 1999). The configuration was forced at the air-sea interface with version 5.2 of the DRAKKAR forcing set (DFS) (Brodeau et al., 2010). DFS 5.2 is based on ERA40 ... Dataset Sea ice DataCite Metadata Store (German National Library of Science and Technology) Medusa ENVELOPE(157.417,157.417,-79.633,-79.633) |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
marine biogeochemistry marine biogeochemistry ocean model MEDUSA NEMO hindcast simulation seafloor organic carbon flux |
spellingShingle |
marine biogeochemistry marine biogeochemistry ocean model MEDUSA NEMO hindcast simulation seafloor organic carbon flux Yool, Andrew Seafloor organic carbon flux output from the NEMO-MEDUSA model ... |
topic_facet |
marine biogeochemistry marine biogeochemistry ocean model MEDUSA NEMO hindcast simulation seafloor organic carbon flux |
description |
This output was produced by a simulation using a coupled ocean physics and marine biogeochemistry model. The physical ocean submodel was the Nucleus for European Modeling of the Ocean (NEMO) physical ocean model (Madec, 2014), run here in a global 1/12-degree resolution configuration (ORCA0083). The marine biogeochemistry submodel was the Model of Ecosystem Dynamics, nutrient Utilisation, Sequestration and Acidification (MEDUSA-2), an intermediate-complexity plankton ecosystem model (Yool et al., 2013). The horizontal resolution of this configuration of NEMO has non-uniform grid cells ranging 2 to 9 km in size (mean 7.5 km), with 75 vertical depth levels (31 levels between the surface and 200 m depth). Sea-ice is represented in the model by the Louvian‐la‐Neuve Ice Model (LIM2) (Fichefet, & Maqueda, M. a. M., 1997; Goosse & Fichefet, 1999). The configuration was forced at the air-sea interface with version 5.2 of the DRAKKAR forcing set (DFS) (Brodeau et al., 2010). DFS 5.2 is based on ERA40 ... |
format |
Dataset |
author |
Yool, Andrew |
author_facet |
Yool, Andrew |
author_sort |
Yool, Andrew |
title |
Seafloor organic carbon flux output from the NEMO-MEDUSA model ... |
title_short |
Seafloor organic carbon flux output from the NEMO-MEDUSA model ... |
title_full |
Seafloor organic carbon flux output from the NEMO-MEDUSA model ... |
title_fullStr |
Seafloor organic carbon flux output from the NEMO-MEDUSA model ... |
title_full_unstemmed |
Seafloor organic carbon flux output from the NEMO-MEDUSA model ... |
title_sort |
seafloor organic carbon flux output from the nemo-medusa model ... |
publisher |
Zenodo |
publishDate |
2022 |
url |
https://dx.doi.org/10.5281/zenodo.6513616 https://zenodo.org/record/6513616 |
long_lat |
ENVELOPE(157.417,157.417,-79.633,-79.633) |
geographic |
Medusa |
geographic_facet |
Medusa |
genre |
Sea ice |
genre_facet |
Sea ice |
op_relation |
https://dx.doi.org/10.5281/zenodo.6513615 |
op_rights |
Open Access Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.5281/zenodo.651361610.5281/zenodo.6513615 |
_version_ |
1768374976733249536 |