Numerical modelling of POC dynamics in the southern Baltic under possible future conditions determined by nutrients, light and temperature

This paper discusses predictions of particulate organic carbon (POC) concentrations in the southern Baltic Sea. The study is based on the one-dimensional Particulate Organic Carbon Model (1D POC), described in detail by Dzierzbicka-Głowacka et al. (2010a). The POC concentration is determined as th...

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Main Authors: Lidia Dzierzbicka-Głowacka, Karol Kuliński, Anna Maciejewska, Jaromir Jakacki, Janusz Pempkowiak
Format: Article
Language:English
Published: Elsevier 2011-11-01
Series:Oceanologia
Subjects:
Online Access:http://www.iopan.gda.pl/oceanologia/53_4.html#A4
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author Lidia Dzierzbicka-Głowacka
Karol Kuliński
Anna Maciejewska
Jaromir Jakacki
Janusz Pempkowiak
author_facet Lidia Dzierzbicka-Głowacka
Karol Kuliński
Anna Maciejewska
Jaromir Jakacki
Janusz Pempkowiak
author_sort Lidia Dzierzbicka-Głowacka
collection DOAJ
description This paper discusses predictions of particulate organic carbon (POC) concentrations in the southern Baltic Sea. The study is based on the one-dimensional Particulate Organic Carbon Model (1D POC), described in detail by Dzierzbicka-Głowacka et al. (2010a). The POC concentration is determined as the sum of phytoplankton, zooplankton and dead organic matter (detritus) concentrations. Temporal changes in the phytoplankton biomass are caused by primary production, mortality, grazing by zooplankton and sinking. The zooplankton biomass is affected by ingestion, excretion, faecal production, mortality and carnivorous grazing. The changes in the pelagic detritus concentration are determined by the input of dead phytoplankton and zooplankton, the natural mortality of predators, faecal pellets, and sinks - sedimentation, zooplankton grazing and biochemical decomposition. The model simulations were done for selected locations in the southern Baltic Sea (Gdańsk Deep, Bornholm Deep and Gotland Deep) under predicted conditions characterized by changes of temperature, nutrient concentrations and light availability. The results cover the daily, monthly, seasonal and annual POC concentration patterns in the upper water layer. If the assumed trends in light, nutrients and temperature in the southern Baltic correctly predict the conditions in 2050, our calculations indicate that we can expect a two- to three-fold increase in POC concentration in late spring and a shift towards postponed maximum POC concentration. It can also be anticipated that, as a result of the increase in POC, oxygenation of the water layer beneath the halocline will decrease, while the supply of food to organisms at higher trophic levels will increase.
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spelling doaj.art-9d6a90928efd4ee7b3ce561d93363a7a2022-12-22T00:46:46ZengElsevierOceanologia0078-32342011-11-01534971992Numerical modelling of POC dynamics in the southern Baltic under possible future conditions determined by nutrients, light and temperatureLidia Dzierzbicka-GłowackaKarol KulińskiAnna MaciejewskaJaromir JakackiJanusz PempkowiakThis paper discusses predictions of particulate organic carbon (POC) concentrations in the southern Baltic Sea. The study is based on the one-dimensional Particulate Organic Carbon Model (1D POC), described in detail by Dzierzbicka-Głowacka et al. (2010a). The POC concentration is determined as the sum of phytoplankton, zooplankton and dead organic matter (detritus) concentrations. Temporal changes in the phytoplankton biomass are caused by primary production, mortality, grazing by zooplankton and sinking. The zooplankton biomass is affected by ingestion, excretion, faecal production, mortality and carnivorous grazing. The changes in the pelagic detritus concentration are determined by the input of dead phytoplankton and zooplankton, the natural mortality of predators, faecal pellets, and sinks - sedimentation, zooplankton grazing and biochemical decomposition. The model simulations were done for selected locations in the southern Baltic Sea (Gdańsk Deep, Bornholm Deep and Gotland Deep) under predicted conditions characterized by changes of temperature, nutrient concentrations and light availability. The results cover the daily, monthly, seasonal and annual POC concentration patterns in the upper water layer. If the assumed trends in light, nutrients and temperature in the southern Baltic correctly predict the conditions in 2050, our calculations indicate that we can expect a two- to three-fold increase in POC concentration in late spring and a shift towards postponed maximum POC concentration. It can also be anticipated that, as a result of the increase in POC, oxygenation of the water layer beneath the halocline will decrease, while the supply of food to organisms at higher trophic levels will increase.http://www.iopan.gda.pl/oceanologia/53_4.html#A4POC modellingPhytoplanktonZooplanktonDetritus
spellingShingle Lidia Dzierzbicka-Głowacka
Karol Kuliński
Anna Maciejewska
Jaromir Jakacki
Janusz Pempkowiak
Numerical modelling of POC dynamics in the southern Baltic under possible future conditions determined by nutrients, light and temperature
Oceanologia
POC modelling
Phytoplankton
Zooplankton
Detritus
title Numerical modelling of POC dynamics in the southern Baltic under possible future conditions determined by nutrients, light and temperature
title_full Numerical modelling of POC dynamics in the southern Baltic under possible future conditions determined by nutrients, light and temperature
title_fullStr Numerical modelling of POC dynamics in the southern Baltic under possible future conditions determined by nutrients, light and temperature
title_full_unstemmed Numerical modelling of POC dynamics in the southern Baltic under possible future conditions determined by nutrients, light and temperature
title_short Numerical modelling of POC dynamics in the southern Baltic under possible future conditions determined by nutrients, light and temperature
title_sort numerical modelling of poc dynamics in the southern baltic under possible future conditions determined by nutrients light and temperature
topic POC modelling
Phytoplankton
Zooplankton
Detritus
url http://www.iopan.gda.pl/oceanologia/53_4.html#A4
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