Uncertainties in modelling CH<sub>4</sub> emissions from northern wetlands in glacial climates: effect of hydrological model and CH<sub>4</sub> model structure

Berrittella, C.; van Huissteden, J.

doi:https://doi.org/10.5194/cp-5-361-2009

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https://doi.org/10.5194/cp-5-361-2009

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21 Jul 2009

| 21 Jul 2009

Uncertainties in modelling CH₄ emissions from northern wetlands in glacial climates: effect of hydrological model and CH₄ model structure

C. Berrittella and J. van Huissteden

C. Berrittella

Vrije Universiteit, VU-Amsterdam, Faculty of Earth and Life Sciences, Department of Hydrology and Geo-Environmental Sciences, De Boelelaan 1085, 1081 HV, Amsterdam, The Netherlands

J. van Huissteden

Vrije Universiteit, VU-Amsterdam, Faculty of Earth and Life Sciences, Department of Hydrology and Geo-Environmental Sciences, De Boelelaan 1085, 1081 HV, Amsterdam, The Netherlands

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Subject: Greenhouse Gases | Archive: Modelling only | Timescale: Pleistocene

Terrestrial methane emissions from the Last Glacial Maximum to the preindustrial period

Thomas Kleinen, Uwe Mikolajewicz, and Victor Brovkin

Clim. Past, 16, 575–595, https://doi.org/10.5194/cp-16-575-2020,https://doi.org/10.5194/cp-16-575-2020, 2020

Short summary

We investigate the changes in natural methane emissions between the Last Glacial Maximum and preindustrial periods with a methane-enabled version of MPI-ESM. We consider all natural sources of methane except for emissions from wild animals and geological sources. Changes are dominated by changes in tropical wetland emissions, high-latitude wetlands play a secondary role, and all other natural sources are of minor importance. We explain the changes in ice core methane by methane emissions only.

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Uncertainties in modelling CH4 emissions from northern wetlands in glacial climates: effect of hydrological model and CH4 model structure

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Uncertainties in modelling CH₄ emissions from northern wetlands in glacial climates: effect of hydrological model and CH₄ model structure