Modeling regional to global CH4 emissions of boreal and arctic wetlands

International audience Methane (CH 4 ) emission from boreal, arctic and subarctic wetlands constitutes a potentially positive feedback to global climate warming. Many process-based models have been developed, but high uncertainties remain in estimating the amount of CH 4 released from wetlands at th...

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Bibliographic Details
Published in:Global Biogeochemical Cycles
Main Authors: Petrescu, A. M. R., van Beek, L. P. H., van Huissteden, J., Prigent, Catherine, Sachs, T., Corradi, C. A. R., Parmentier, Frans-Jan W., Dolman, A. J.
Other Authors: Department of Hydrology and Geo-Environmental Sciences, Faculty of Earth and Life Sciences, VU University, Department of Physical Geography, Utrecht University, Departement de Radioastronomie Millimétrique (DEMIRM), Observatoire de Paris, Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL), Alfred-Wegener-Institute for Polar and Marine Research (AWI), Laboratory of Forest Ecology, Department of Forest Environment and Resources, University of Tuscia of Viterbo
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2010
Subjects:
Online Access:https://hal.science/hal-03742539
https://doi.org/10.1029/2009GB003610
Description
Summary:International audience Methane (CH 4 ) emission from boreal, arctic and subarctic wetlands constitutes a potentially positive feedback to global climate warming. Many process-based models have been developed, but high uncertainties remain in estimating the amount of CH 4 released from wetlands at the global scale. This study tries to improve estimates of CH 4 emissions by up-scaling a wetland CH 4 emission model, PEATLAND-VU, to the global scale with a spatial resolution of 0.5° for the period 2001-2006. This up-scaling was based on the global circum-arctic distribution of wetlands with hydrological conditions being specified by a global hydrological model, PCR-GLOBWB. In addition to the daily hydrological output from PCR-GLOBWB, comprising water table depths and snow thickness, the parameterization included air temperature as obtained from the ECMWF Operational Archive. To establish the uncertainty in the representations of the circum-arctic distribution of wetlands on the CH 4 emission, several existing products were used to aggregate the emissions. Using the description of potential peatlands from the FAO Digital Soil Map of the World and the representation of floodplains by PCR-GLOBWB, the average annual flux over the period 2001-2006 was estimated to be 78 Tg yr -1 . In comparison, the six-year average CH 4 fluxes were 37.7, 89.4, 145.6, and 157.3 Tg yr -1 for different estimates of wetland extends based on the studies by Matthews and Fung, Prigent et al., Lehner and Döll, and Kaplan, respectively. This study shows the feasibility to estimate interannual variations in CH 4 emissions by coupling hydrological and CH 4 emission process models. It highlights the importance of an adequate understanding of hydrology in quantifying the total emissions from northern hemispheric wetlands and shows how knowledge of the sub-grid variability in wetland extent helps to prescribe relevant hydrological conditions to the emission model as well as to identify the uncertainty associated with existing wetland distributions.