Biological data assimilation for parameter estimation of a phytoplankton functional type model for the western North Pacific

Ecosystem models are used to understand ecosystem dynamics and ocean biogeochemical cycles and require optimum physiological parameters to best represent biological behaviours. These physiological parameters are often tuned up empirically, while ecosystem models have evolved to increase the number o...

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Published in:Ocean Science
Main Authors: Hoshiba, Yasuhiro, Hirata, Takafumi, Shigemitsu, Masahito, Nakano, Hideyuki, Hashioka, Taketo, Masuda, Yoshio, Yamanaka, Yasuhiro
Format: Text
Language:English
Published: 2019
Subjects:
Online Access:https://doi.org/10.5194/os-14-371-2018
https://os.copernicus.org/articles/14/371/2018/
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spelling ftcopernicus:oai:publications.copernicus.org:os58945 2023-05-15T18:28:25+02:00 Biological data assimilation for parameter estimation of a phytoplankton functional type model for the western North Pacific Hoshiba, Yasuhiro Hirata, Takafumi Shigemitsu, Masahito Nakano, Hideyuki Hashioka, Taketo Masuda, Yoshio Yamanaka, Yasuhiro 2019-01-07 application/pdf https://doi.org/10.5194/os-14-371-2018 https://os.copernicus.org/articles/14/371/2018/ eng eng doi:10.5194/os-14-371-2018 https://os.copernicus.org/articles/14/371/2018/ eISSN: 1812-0792 Text 2019 ftcopernicus https://doi.org/10.5194/os-14-371-2018 2020-07-20T16:23:16Z Ecosystem models are used to understand ecosystem dynamics and ocean biogeochemical cycles and require optimum physiological parameters to best represent biological behaviours. These physiological parameters are often tuned up empirically, while ecosystem models have evolved to increase the number of physiological parameters. We developed a three-dimensional (3-D) lower-trophic-level marine ecosystem model known as the Nitrogen, Silicon and Iron regulated Marine Ecosystem Model (NSI-MEM) and employed biological data assimilation using a micro-genetic algorithm to estimate 23 physiological parameters for two phytoplankton functional types in the western North Pacific. The estimation of the parameters was based on a one-dimensional simulation that referenced satellite data for constraining the physiological parameters. The 3-D NSI-MEM optimized by the data assimilation improved the timing of a modelled plankton bloom in the subarctic and subtropical regions compared to the model without data assimilation. Furthermore, the model was able to improve not only surface concentrations of phytoplankton but also their subsurface maximum concentrations. Our results showed that surface data assimilation of physiological parameters from two contrasting observatory stations benefits the representation of vertical plankton distribution in the western North Pacific. Text Subarctic Copernicus Publications: E-Journals Pacific Ocean Science 14 3 371 386
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description Ecosystem models are used to understand ecosystem dynamics and ocean biogeochemical cycles and require optimum physiological parameters to best represent biological behaviours. These physiological parameters are often tuned up empirically, while ecosystem models have evolved to increase the number of physiological parameters. We developed a three-dimensional (3-D) lower-trophic-level marine ecosystem model known as the Nitrogen, Silicon and Iron regulated Marine Ecosystem Model (NSI-MEM) and employed biological data assimilation using a micro-genetic algorithm to estimate 23 physiological parameters for two phytoplankton functional types in the western North Pacific. The estimation of the parameters was based on a one-dimensional simulation that referenced satellite data for constraining the physiological parameters. The 3-D NSI-MEM optimized by the data assimilation improved the timing of a modelled plankton bloom in the subarctic and subtropical regions compared to the model without data assimilation. Furthermore, the model was able to improve not only surface concentrations of phytoplankton but also their subsurface maximum concentrations. Our results showed that surface data assimilation of physiological parameters from two contrasting observatory stations benefits the representation of vertical plankton distribution in the western North Pacific.
format Text
author Hoshiba, Yasuhiro
Hirata, Takafumi
Shigemitsu, Masahito
Nakano, Hideyuki
Hashioka, Taketo
Masuda, Yoshio
Yamanaka, Yasuhiro
spellingShingle Hoshiba, Yasuhiro
Hirata, Takafumi
Shigemitsu, Masahito
Nakano, Hideyuki
Hashioka, Taketo
Masuda, Yoshio
Yamanaka, Yasuhiro
Biological data assimilation for parameter estimation of a phytoplankton functional type model for the western North Pacific
author_facet Hoshiba, Yasuhiro
Hirata, Takafumi
Shigemitsu, Masahito
Nakano, Hideyuki
Hashioka, Taketo
Masuda, Yoshio
Yamanaka, Yasuhiro
author_sort Hoshiba, Yasuhiro
title Biological data assimilation for parameter estimation of a phytoplankton functional type model for the western North Pacific
title_short Biological data assimilation for parameter estimation of a phytoplankton functional type model for the western North Pacific
title_full Biological data assimilation for parameter estimation of a phytoplankton functional type model for the western North Pacific
title_fullStr Biological data assimilation for parameter estimation of a phytoplankton functional type model for the western North Pacific
title_full_unstemmed Biological data assimilation for parameter estimation of a phytoplankton functional type model for the western North Pacific
title_sort biological data assimilation for parameter estimation of a phytoplankton functional type model for the western north pacific
publishDate 2019
url https://doi.org/10.5194/os-14-371-2018
https://os.copernicus.org/articles/14/371/2018/
geographic Pacific
geographic_facet Pacific
genre Subarctic
genre_facet Subarctic
op_source eISSN: 1812-0792
op_relation doi:10.5194/os-14-371-2018
https://os.copernicus.org/articles/14/371/2018/
op_doi https://doi.org/10.5194/os-14-371-2018
container_title Ocean Science
container_volume 14
container_issue 3
container_start_page 371
op_container_end_page 386
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