Modelling a simple mechanism for the formation of phytoplankton thin layers using large-eddy simulation: in situ growth

Publikation: Beitrag in FachzeitschriftArtikelForschungPeer-Review

Autoren

  • Ashley Brereton
  • Yign Noh
  • Siegfried Raasch

Externe Organisationen

  • Yonsei University
Forschungs-netzwerk anzeigen

Details

OriginalspracheEnglisch
Seiten (von - bis)77-90
Seitenumfang14
FachzeitschriftMarine ecology progress series
Jahrgang653
PublikationsstatusVeröffentlicht - 29 Okt. 2020

Abstract

A curious phenomenon found in phytoplankton communities is the forming of so-called thin layers, wherein phytoplankton biomass can stretch out kilometres in the horizontal but only a few metres in the vertical. These layers are typically found at the pycnocline, just below the surface mixed layer. Thin layers are usually attributed to a range of complex environmental and species-dependent factors. However, we believe that, given the frequency at which this phenomenon is observed, a simpler mechanism is at play. In this study, we found that phytoplankton thin layers can be attributed simply to a decreasing light availability with depth, when there is an abundance of nutrients in the euphotic zone and below the mixed layer. This mechanism was ascertained using a number of modelling approaches ranging in complexity from analytical solutions of a simple 1-dimensional plankton model to a 3-dimensional biophysical model incorporating large-eddy simulation. The conditions which, according to the results of our study, allow thin layers to form are ubiquitous in the coastal ocean and are therefore a likely candidate explanation as to why planktonic thin layers are so frequently observed.

ASJC Scopus Sachgebiete

Zitieren

Modelling a simple mechanism for the formation of phytoplankton thin layers using large-eddy simulation: in situ growth. / Brereton, Ashley; Noh, Yign; Raasch, Siegfried.
in: Marine ecology progress series, Jahrgang 653, 29.10.2020, S. 77-90.

Publikation: Beitrag in FachzeitschriftArtikelForschungPeer-Review

Download
@article{cd088c2d489b448ebeabdf0c1225ff6b,
title = "Modelling a simple mechanism for the formation of phytoplankton thin layers using large-eddy simulation: in situ growth",
abstract = "A curious phenomenon found in phytoplankton communities is the forming of so-called thin layers, wherein phytoplankton biomass can stretch out kilometres in the horizontal but only a few metres in the vertical. These layers are typically found at the pycnocline, just below the surface mixed layer. Thin layers are usually attributed to a range of complex environmental and species-dependent factors. However, we believe that, given the frequency at which this phenomenon is observed, a simpler mechanism is at play. In this study, we found that phytoplankton thin layers can be attributed simply to a decreasing light availability with depth, when there is an abundance of nutrients in the euphotic zone and below the mixed layer. This mechanism was ascertained using a number of modelling approaches ranging in complexity from analytical solutions of a simple 1-dimensional plankton model to a 3-dimensional biophysical model incorporating large-eddy simulation. The conditions which, according to the results of our study, allow thin layers to form are ubiquitous in the coastal ocean and are therefore a likely candidate explanation as to why planktonic thin layers are so frequently observed.",
keywords = "Biophysical modelling, Large-eddy simulation, Mixed layer turbulence, Particle modelling, Plankton thin layers",
author = "Ashley Brereton and Yign Noh and Siegfried Raasch",
note = "Funding information:. This work was supported by the Korea Meteorological Administration Research and Development Program under grant KMI2018-07210. We are also grateful for support from the PycnMix project (NE/L003325/1). This work used the ARCHER UK National Supercomputing Service. We are extremely grateful to Prof. Peter Franks for important criticisms on an earlier version of the model, which guided the present study considerably. We are also thankful to Dr David Lewis for valuable discussions concerning the modeling work and to the 2 anonymous reviewers who provided constructive feedback, which helped to improve the manuscript significantly.",
year = "2020",
month = oct,
day = "29",
doi = "10.3354/meps13471",
language = "English",
volume = "653",
pages = "77--90",
journal = "Marine ecology progress series",
issn = "0171-8630",
publisher = "Inter-Research",

}

Download

TY - JOUR

T1 - Modelling a simple mechanism for the formation of phytoplankton thin layers using large-eddy simulation: in situ growth

AU - Brereton, Ashley

AU - Noh, Yign

AU - Raasch, Siegfried

N1 - Funding information:. This work was supported by the Korea Meteorological Administration Research and Development Program under grant KMI2018-07210. We are also grateful for support from the PycnMix project (NE/L003325/1). This work used the ARCHER UK National Supercomputing Service. We are extremely grateful to Prof. Peter Franks for important criticisms on an earlier version of the model, which guided the present study considerably. We are also thankful to Dr David Lewis for valuable discussions concerning the modeling work and to the 2 anonymous reviewers who provided constructive feedback, which helped to improve the manuscript significantly.

PY - 2020/10/29

Y1 - 2020/10/29

N2 - A curious phenomenon found in phytoplankton communities is the forming of so-called thin layers, wherein phytoplankton biomass can stretch out kilometres in the horizontal but only a few metres in the vertical. These layers are typically found at the pycnocline, just below the surface mixed layer. Thin layers are usually attributed to a range of complex environmental and species-dependent factors. However, we believe that, given the frequency at which this phenomenon is observed, a simpler mechanism is at play. In this study, we found that phytoplankton thin layers can be attributed simply to a decreasing light availability with depth, when there is an abundance of nutrients in the euphotic zone and below the mixed layer. This mechanism was ascertained using a number of modelling approaches ranging in complexity from analytical solutions of a simple 1-dimensional plankton model to a 3-dimensional biophysical model incorporating large-eddy simulation. The conditions which, according to the results of our study, allow thin layers to form are ubiquitous in the coastal ocean and are therefore a likely candidate explanation as to why planktonic thin layers are so frequently observed.

AB - A curious phenomenon found in phytoplankton communities is the forming of so-called thin layers, wherein phytoplankton biomass can stretch out kilometres in the horizontal but only a few metres in the vertical. These layers are typically found at the pycnocline, just below the surface mixed layer. Thin layers are usually attributed to a range of complex environmental and species-dependent factors. However, we believe that, given the frequency at which this phenomenon is observed, a simpler mechanism is at play. In this study, we found that phytoplankton thin layers can be attributed simply to a decreasing light availability with depth, when there is an abundance of nutrients in the euphotic zone and below the mixed layer. This mechanism was ascertained using a number of modelling approaches ranging in complexity from analytical solutions of a simple 1-dimensional plankton model to a 3-dimensional biophysical model incorporating large-eddy simulation. The conditions which, according to the results of our study, allow thin layers to form are ubiquitous in the coastal ocean and are therefore a likely candidate explanation as to why planktonic thin layers are so frequently observed.

KW - Biophysical modelling

KW - Large-eddy simulation

KW - Mixed layer turbulence

KW - Particle modelling

KW - Plankton thin layers

UR - http://www.scopus.com/inward/record.url?scp=85095739501&partnerID=8YFLogxK

U2 - 10.3354/meps13471

DO - 10.3354/meps13471

M3 - Article

AN - SCOPUS:85095739501

VL - 653

SP - 77

EP - 90

JO - Marine ecology progress series

JF - Marine ecology progress series

SN - 0171-8630

ER -