A stochastic, Lagrangian model of sinking biogenic aggregates in the ocean (SLAMS 1.0): model formulation, validation and sensitivity

We present a new mechanistic model, stochastic, Lagrangian aggregate model of sinking particles (SLAMS) for the biological pump in the ocean, which tracks the evolution of individual particles as they aggregate, disaggregate, sink, and are altered by chemical and biological processes. SLAMS consider...

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Main Authors: T. Jokulsdottir, D. Archer
Format: Article
Language:English
Published: Copernicus Publications 2016-04-01
Series:Geoscientific Model Development
Online Access:http://www.geosci-model-dev.net/9/1455/2016/gmd-9-1455-2016.pdf
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spelling doaj-10cfd6cdcee042f09861a027ea5481292020-11-25T00:19:44ZengCopernicus PublicationsGeoscientific Model Development1991-959X1991-96032016-04-01941455147610.5194/gmd-9-1455-2016A stochastic, Lagrangian model of sinking biogenic aggregates in the ocean (SLAMS 1.0): model formulation, validation and sensitivityT. Jokulsdottir0D. Archer1Department of the Geophysical Sciences, University of Chicago, Chicago, IL 60637, USADepartment of the Geophysical Sciences, University of Chicago, Chicago, IL 60637, USAWe present a new mechanistic model, stochastic, Lagrangian aggregate model of sinking particles (SLAMS) for the biological pump in the ocean, which tracks the evolution of individual particles as they aggregate, disaggregate, sink, and are altered by chemical and biological processes. SLAMS considers the impacts of ballasting by mineral phases, binding of aggregates by transparent exopolymer particles (TEP), zooplankton grazing and the fractal geometry (porosity) of the aggregates. Parameterizations for age-dependent organic carbon (orgC) degradation kinetics, and disaggregation driven by zooplankton grazing and TEP degradation, are motivated by observed particle fluxes and size spectra throughout the water column. The model is able to explain observed variations in orgC export efficiency and rain ratio from the euphotic zone and to the sea floor as driven by sea surface temperature and the primary production rate and seasonality of primary production. The model provides a new mechanistic framework with which to predict future changes on the flux attenuation of orgC in response to climate change forcing.http://www.geosci-model-dev.net/9/1455/2016/gmd-9-1455-2016.pdf
collection DOAJ
language English
format Article
sources DOAJ
author T. Jokulsdottir
D. Archer
spellingShingle T. Jokulsdottir
D. Archer
A stochastic, Lagrangian model of sinking biogenic aggregates in the ocean (SLAMS 1.0): model formulation, validation and sensitivity
Geoscientific Model Development
author_facet T. Jokulsdottir
D. Archer
author_sort T. Jokulsdottir
title A stochastic, Lagrangian model of sinking biogenic aggregates in the ocean (SLAMS 1.0): model formulation, validation and sensitivity
title_short A stochastic, Lagrangian model of sinking biogenic aggregates in the ocean (SLAMS 1.0): model formulation, validation and sensitivity
title_full A stochastic, Lagrangian model of sinking biogenic aggregates in the ocean (SLAMS 1.0): model formulation, validation and sensitivity
title_fullStr A stochastic, Lagrangian model of sinking biogenic aggregates in the ocean (SLAMS 1.0): model formulation, validation and sensitivity
title_full_unstemmed A stochastic, Lagrangian model of sinking biogenic aggregates in the ocean (SLAMS 1.0): model formulation, validation and sensitivity
title_sort stochastic, lagrangian model of sinking biogenic aggregates in the ocean (slams 1.0): model formulation, validation and sensitivity
publisher Copernicus Publications
series Geoscientific Model Development
issn 1991-959X
1991-9603
publishDate 2016-04-01
description We present a new mechanistic model, stochastic, Lagrangian aggregate model of sinking particles (SLAMS) for the biological pump in the ocean, which tracks the evolution of individual particles as they aggregate, disaggregate, sink, and are altered by chemical and biological processes. SLAMS considers the impacts of ballasting by mineral phases, binding of aggregates by transparent exopolymer particles (TEP), zooplankton grazing and the fractal geometry (porosity) of the aggregates. Parameterizations for age-dependent organic carbon (orgC) degradation kinetics, and disaggregation driven by zooplankton grazing and TEP degradation, are motivated by observed particle fluxes and size spectra throughout the water column. The model is able to explain observed variations in orgC export efficiency and rain ratio from the euphotic zone and to the sea floor as driven by sea surface temperature and the primary production rate and seasonality of primary production. The model provides a new mechanistic framework with which to predict future changes on the flux attenuation of orgC in response to climate change forcing.
url http://www.geosci-model-dev.net/9/1455/2016/gmd-9-1455-2016.pdf
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