Sensitivity of phytoplankton distributions to vertical mixing along a North Atlantic transect

Using in situ data of upper ocean vertical mixing along a transect in the North Atlantic and a one-dimensional phytoplankton growth model, we study the sensitivity of the surface phytoplankton concentration to vertical mixing distributions. The study is divided into two parts. In the first part, the...

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Main Authors: L. Hahn-Woernle, H. A. Dijkstra, H. J. Van der Woerd
Format: Article
Language:English
Published: Copernicus Publications 2014-12-01
Series:Ocean Science
Online Access:http://www.ocean-sci.net/10/993/2014/os-10-993-2014.pdf
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spelling doaj-f8fad6c2a7014c4eba7dac50881a5cdd2020-11-25T01:27:13ZengCopernicus PublicationsOcean Science1812-07841812-07922014-12-01106993101110.5194/os-10-993-2014Sensitivity of phytoplankton distributions to vertical mixing along a North Atlantic transectL. Hahn-Woernle0H. A. Dijkstra1H. J. Van der Woerd2Institute for Marine and Atmospheric Research Utrecht (IMAU), Dept. of Physics and Astronomy, Utrecht University, P.O. Box 80.005, 3508 TA Utrecht, the NetherlandsInstitute for Marine and Atmospheric Research Utrecht (IMAU), Dept. of Physics and Astronomy, Utrecht University, P.O. Box 80.005, 3508 TA Utrecht, the NetherlandsInstitute for Environmental Studies (IVM), Free University of Amsterdam, the NetherlandsUsing in situ data of upper ocean vertical mixing along a transect in the North Atlantic and a one-dimensional phytoplankton growth model, we study the sensitivity of the surface phytoplankton concentration to vertical mixing distributions. The study is divided into two parts. In the first part, the model is calibrated to the observations. The optical model parameters are determined from measurements of the light attenuation. The biological parameters are calibrated to three different reference stations with observed vertical profiles of the chlorophyll <i>a</i> (Chl <i>a</i>) concentration and the nutrient concentration. In the second part, the sensitivity of the three model calibrations to the vertical mixing is studied. Therefore measured vertical mixing profiles are applied to the model. These mixing profiles are based on the measurements along the transect and are treated as a set of possible mixing situations of the North Atlantic. Results show that shifts in vertical mixing are able to induce a transition from an upper chlorophyll maximum to a deep one and vice versa. Furthermore, a clear correlation between the surface phytoplankton concentration and the mixing induced nutrient flux is found for nutrient-limited cases. This may open up the possibility to extract characteristics of vertical mixing from satellite ocean colour data using data-assimilation methods.http://www.ocean-sci.net/10/993/2014/os-10-993-2014.pdf
collection DOAJ
language English
format Article
sources DOAJ
author L. Hahn-Woernle
H. A. Dijkstra
H. J. Van der Woerd
spellingShingle L. Hahn-Woernle
H. A. Dijkstra
H. J. Van der Woerd
Sensitivity of phytoplankton distributions to vertical mixing along a North Atlantic transect
Ocean Science
author_facet L. Hahn-Woernle
H. A. Dijkstra
H. J. Van der Woerd
author_sort L. Hahn-Woernle
title Sensitivity of phytoplankton distributions to vertical mixing along a North Atlantic transect
title_short Sensitivity of phytoplankton distributions to vertical mixing along a North Atlantic transect
title_full Sensitivity of phytoplankton distributions to vertical mixing along a North Atlantic transect
title_fullStr Sensitivity of phytoplankton distributions to vertical mixing along a North Atlantic transect
title_full_unstemmed Sensitivity of phytoplankton distributions to vertical mixing along a North Atlantic transect
title_sort sensitivity of phytoplankton distributions to vertical mixing along a north atlantic transect
publisher Copernicus Publications
series Ocean Science
issn 1812-0784
1812-0792
publishDate 2014-12-01
description Using in situ data of upper ocean vertical mixing along a transect in the North Atlantic and a one-dimensional phytoplankton growth model, we study the sensitivity of the surface phytoplankton concentration to vertical mixing distributions. The study is divided into two parts. In the first part, the model is calibrated to the observations. The optical model parameters are determined from measurements of the light attenuation. The biological parameters are calibrated to three different reference stations with observed vertical profiles of the chlorophyll <i>a</i> (Chl <i>a</i>) concentration and the nutrient concentration. In the second part, the sensitivity of the three model calibrations to the vertical mixing is studied. Therefore measured vertical mixing profiles are applied to the model. These mixing profiles are based on the measurements along the transect and are treated as a set of possible mixing situations of the North Atlantic. Results show that shifts in vertical mixing are able to induce a transition from an upper chlorophyll maximum to a deep one and vice versa. Furthermore, a clear correlation between the surface phytoplankton concentration and the mixing induced nutrient flux is found for nutrient-limited cases. This may open up the possibility to extract characteristics of vertical mixing from satellite ocean colour data using data-assimilation methods.
url http://www.ocean-sci.net/10/993/2014/os-10-993-2014.pdf
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