MESMO 3: Flexible phytoplankton stoichiometry and refractory dissolved organic matter

<p>We describe the third version of Minnesota Earth System Model for Ocean biogeochemistry (MESMO 3), an Earth system model of intermediate complexity, with a dynamical ocean, dynamic–thermodynamic sea ice, and an energy–moisture-balanced atmosphere. A major feature of version 3 is the flexibl...

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Main Authors: K. Matsumoto, T. Tanioka, J. Zahn
Format: Article
Language:English
Published: Copernicus Publications 2021-04-01
Series:Geoscientific Model Development
Online Access:https://gmd.copernicus.org/articles/14/2265/2021/gmd-14-2265-2021.pdf
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author K. Matsumoto
T. Tanioka
T. Tanioka
J. Zahn
author_facet K. Matsumoto
T. Tanioka
T. Tanioka
J. Zahn
author_sort K. Matsumoto
collection DOAJ
description <p>We describe the third version of Minnesota Earth System Model for Ocean biogeochemistry (MESMO 3), an Earth system model of intermediate complexity, with a dynamical ocean, dynamic–thermodynamic sea ice, and an energy–moisture-balanced atmosphere. A major feature of version 3 is the flexible <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M1" display="inline" overflow="scroll" dspmath="mathml"><mrow class="chem"><mi mathvariant="normal">C</mi><mo>:</mo><mi mathvariant="normal">N</mi><mo>:</mo><mi mathvariant="normal">P</mi></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="41pt" height="10pt" class="svg-formula" dspmath="mathimg" md5hash="89baeb1bef20dd832e5430c0fb7046a4"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="gmd-14-2265-2021-ie00001.svg" width="41pt" height="10pt" src="gmd-14-2265-2021-ie00001.png"/></svg:svg></span></span> ratio for the three phytoplankton functional types represented in the model. The flexible stoichiometry is based on the power law formulation with environmental dependence on phosphate, nitrate, temperature, and light. Other new features include nitrogen fixation, water column denitrification, oxygen and temperature-dependent organic matter remineralization, and CaCO<span class="inline-formula"><sub>3</sub></span> production based on the concept of the residual nitrate potential growth. In addition, we describe the semi-labile and refractory dissolved organic pools of C, N, P, and Fe that can be enabled in MESMO 3 as an optional feature. The refractory dissolved organic matter can be degraded by photodegradation at the surface and hydrothermal vent degradation at the bottom. These improvements provide a basis for using MESMO 3 in further investigations of the global marine carbon cycle to changes in the environmental conditions of the past, present, and future.</p>
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spelling doaj.art-d6657e16b30e4686b57bad4a1eb329942022-12-21T22:28:02ZengCopernicus PublicationsGeoscientific Model Development1991-959X1991-96032021-04-01142265228810.5194/gmd-14-2265-2021MESMO 3: Flexible phytoplankton stoichiometry and refractory dissolved organic matterK. Matsumoto0T. Tanioka1T. Tanioka2J. Zahn3Department of Earth & Environmental Sciences, University of Minnesota, Minneapolis, Minnesota, USADepartment of Earth & Environmental Sciences, University of Minnesota, Minneapolis, Minnesota, USAcurrent affiliation: Department of Earth System Science, University of California Irvine, Irvine, California, USADepartment of Earth & Environmental Sciences, University of Minnesota, Minneapolis, Minnesota, USA<p>We describe the third version of Minnesota Earth System Model for Ocean biogeochemistry (MESMO 3), an Earth system model of intermediate complexity, with a dynamical ocean, dynamic–thermodynamic sea ice, and an energy–moisture-balanced atmosphere. A major feature of version 3 is the flexible <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M1" display="inline" overflow="scroll" dspmath="mathml"><mrow class="chem"><mi mathvariant="normal">C</mi><mo>:</mo><mi mathvariant="normal">N</mi><mo>:</mo><mi mathvariant="normal">P</mi></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="41pt" height="10pt" class="svg-formula" dspmath="mathimg" md5hash="89baeb1bef20dd832e5430c0fb7046a4"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="gmd-14-2265-2021-ie00001.svg" width="41pt" height="10pt" src="gmd-14-2265-2021-ie00001.png"/></svg:svg></span></span> ratio for the three phytoplankton functional types represented in the model. The flexible stoichiometry is based on the power law formulation with environmental dependence on phosphate, nitrate, temperature, and light. Other new features include nitrogen fixation, water column denitrification, oxygen and temperature-dependent organic matter remineralization, and CaCO<span class="inline-formula"><sub>3</sub></span> production based on the concept of the residual nitrate potential growth. In addition, we describe the semi-labile and refractory dissolved organic pools of C, N, P, and Fe that can be enabled in MESMO 3 as an optional feature. The refractory dissolved organic matter can be degraded by photodegradation at the surface and hydrothermal vent degradation at the bottom. These improvements provide a basis for using MESMO 3 in further investigations of the global marine carbon cycle to changes in the environmental conditions of the past, present, and future.</p>https://gmd.copernicus.org/articles/14/2265/2021/gmd-14-2265-2021.pdf
spellingShingle K. Matsumoto
T. Tanioka
T. Tanioka
J. Zahn
MESMO 3: Flexible phytoplankton stoichiometry and refractory dissolved organic matter
Geoscientific Model Development
title MESMO 3: Flexible phytoplankton stoichiometry and refractory dissolved organic matter
title_full MESMO 3: Flexible phytoplankton stoichiometry and refractory dissolved organic matter
title_fullStr MESMO 3: Flexible phytoplankton stoichiometry and refractory dissolved organic matter
title_full_unstemmed MESMO 3: Flexible phytoplankton stoichiometry and refractory dissolved organic matter
title_short MESMO 3: Flexible phytoplankton stoichiometry and refractory dissolved organic matter
title_sort mesmo 3 flexible phytoplankton stoichiometry and refractory dissolved organic matter
url https://gmd.copernicus.org/articles/14/2265/2021/gmd-14-2265-2021.pdf
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