Explaining the seasonal cycle of the globally averaged CO<sub>2</sub> with a carbon-cycle model

The seasonal changes in the globally averaged atmospheric carbon-dioxide concentrations reflect an important aspect of the global carbon cycle: the gas exchange between the atmosphere and terrestrial biosphere. The data on the globally averaged atmospheric carbon-dioxide concentrations, which are re...

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Main Author: G. A. Alexandrov
Format: Article
Language:English
Published: Copernicus Publications 2014-10-01
Series:Earth System Dynamics
Online Access:http://www.earth-syst-dynam.net/5/345/2014/esd-5-345-2014.pdf
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spelling doaj-5b5e642f6c614124851008718c9547b42020-11-24T21:42:16ZengCopernicus PublicationsEarth System Dynamics2190-49792190-49872014-10-015234535410.5194/esd-5-345-2014Explaining the seasonal cycle of the globally averaged CO<sub>2</sub> with a carbon-cycle modelG. A. Alexandrov0A. M. Obukhov Institute of Atmospheric Physics, Russian Academy of Sciences, Pyzhevsky 3, 119017 Moscow, RussiaThe seasonal changes in the globally averaged atmospheric carbon-dioxide concentrations reflect an important aspect of the global carbon cycle: the gas exchange between the atmosphere and terrestrial biosphere. The data on the globally averaged atmospheric carbon-dioxide concentrations, which are reported by Earth System Research Laboratory of the US National Oceanic & Atmospheric Administration (NOAA/ESRL), could be used to demonstrate the adequacy of the global carbon-cycle models. However, it was recently found that the observed amplitude of seasonal variations in the atmospheric carbon-dioxide concentrations is higher than simulated. In this paper, the factors that affect the amplitude of seasonal variations are explored using a carbon-cycle model of reduced complexity. The model runs show that the low amplitude of the simulated seasonal variations may result from underestimated effect of substrate limitation on the seasonal pattern of heterotrophic respiration and from an underestimated magnitude of the annual gross primary production (GPP) in the terrestrial ecosystems located to the north of 25° N.http://www.earth-syst-dynam.net/5/345/2014/esd-5-345-2014.pdf
collection DOAJ
language English
format Article
sources DOAJ
author G. A. Alexandrov
spellingShingle G. A. Alexandrov
Explaining the seasonal cycle of the globally averaged CO<sub>2</sub> with a carbon-cycle model
Earth System Dynamics
author_facet G. A. Alexandrov
author_sort G. A. Alexandrov
title Explaining the seasonal cycle of the globally averaged CO<sub>2</sub> with a carbon-cycle model
title_short Explaining the seasonal cycle of the globally averaged CO<sub>2</sub> with a carbon-cycle model
title_full Explaining the seasonal cycle of the globally averaged CO<sub>2</sub> with a carbon-cycle model
title_fullStr Explaining the seasonal cycle of the globally averaged CO<sub>2</sub> with a carbon-cycle model
title_full_unstemmed Explaining the seasonal cycle of the globally averaged CO<sub>2</sub> with a carbon-cycle model
title_sort explaining the seasonal cycle of the globally averaged co<sub>2</sub> with a carbon-cycle model
publisher Copernicus Publications
series Earth System Dynamics
issn 2190-4979
2190-4987
publishDate 2014-10-01
description The seasonal changes in the globally averaged atmospheric carbon-dioxide concentrations reflect an important aspect of the global carbon cycle: the gas exchange between the atmosphere and terrestrial biosphere. The data on the globally averaged atmospheric carbon-dioxide concentrations, which are reported by Earth System Research Laboratory of the US National Oceanic & Atmospheric Administration (NOAA/ESRL), could be used to demonstrate the adequacy of the global carbon-cycle models. However, it was recently found that the observed amplitude of seasonal variations in the atmospheric carbon-dioxide concentrations is higher than simulated. In this paper, the factors that affect the amplitude of seasonal variations are explored using a carbon-cycle model of reduced complexity. The model runs show that the low amplitude of the simulated seasonal variations may result from underestimated effect of substrate limitation on the seasonal pattern of heterotrophic respiration and from an underestimated magnitude of the annual gross primary production (GPP) in the terrestrial ecosystems located to the north of 25° N.
url http://www.earth-syst-dynam.net/5/345/2014/esd-5-345-2014.pdf
work_keys_str_mv AT gaalexandrov explainingtheseasonalcycleofthegloballyaveragedcosub2subwithacarboncyclemodel
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