Monthly gridded data product of northern wetland methane emissions based on upscaling eddy covariance observations
Olli Peltola, Timo Vesala, Yao Gao, Olle Räty, Pavel Alekseychik, Mika Aurela, Bogdan H. Chojnicki, Ankur R. Desai, A. J. Dolman, E. S. Euskirchen, Thomas Friborg, Mathias Göckede, Manuel Helbig, Elyn Humphreys, Robert B. Jackson, Georg Jocher, Fortunat Joos, Janina Klatt, Sara Knox, Natalia Kowalska, Lars Kutzbach, Sebastian Lienert, Annalea Lohila, Ivan Mammarella, Daniel F. Nadeau, Mats B. Nilsson, Walter C. Oechel, Matthias Peichl, Thomas G. Pypker, W. L. Quinton, Janne Rinne, Torsten Sachs, Mateusz Samson, Hans Peter Schmid, Oliver Sonnentag, Christian Wille, Donatella Zona, Tuula Aalto
Abstract
Abstract. Natural wetlands constitute the largest and most uncertain source of methane (CH4) to the atmosphere and a large fraction of them are found in the northern latitudes. These emissions are typically estimated using process (“bottom-up”) or inversion (“top-down”) models. However, estimates from these two types of models are not independent of each other since the top-down estimates usually rely on the a priori estimation of these emissions obtained with process models. Hence, independent spatially explicit validation data are needed. Here we utilize a random forest (RF) machine-learning technique to upscale CH4 eddy covariance flux measurements from 25 sites to estimate CH4 wetland emissions from the northern latitudes (north of 45∘ N). Eddy covariance data from 2005 to 2016 are used for model development. The model is then used to predict emissions during 2013 and 2014. The predictive performance of the RF model is evaluated using a leave-one-site-out cross-validation scheme. The performance (Nash–Sutcliffe model efficiency =0.47) is comparable to previous studies upscaling net ecosystem exchange of carbon dioxide and studies comparing process model output against site-level CH4 emission data. The global distribution of wetlands is one major source of uncertainty for upscaling CH4. Thus, three wetland distribution maps are utilized in the upscaling. Depending on the wetland distribution map, the annual emissions for the northern wetlands yield 32 (22.3–41.2, 95 % confidence interval calculated from a RF model ensemble), 31 (21.4–39.9) or 38 (25.9–49.5) Tg(CH4) yr−1. To further evaluate the uncertainties of the upscaled CH4 flux data products we also compared them against output from two process models (LPX-Bern and WetCHARTs), and methodological issues related to CH4 flux upscaling are discussed. The monthly upscaled CH4 flux data products are available at https://doi.org/10.5281/zenodo.2560163 (Peltola et al., 2019).- Cite:
- Olli Peltola, Timo Vesala, Yao Gao, Olle Räty, Pavel Alekseychik, Mika Aurela, Bogdan H. Chojnicki, Ankur R. Desai, A. J. Dolman, E. S. Euskirchen, Thomas Friborg, Mathias Göckede, Manuel Helbig, Elyn Humphreys, Robert B. Jackson, Georg Jocher, Fortunat Joos, Janina Klatt, Sara Knox, et al.. 2019. Monthly gridded data product of northern wetland methane emissions based on upscaling eddy covariance observations. Earth System Science Data, Volume 11, Issue 3, 11(3):1263–1289.
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@article{Peltola-2019-Monthly,
title = "Monthly gridded data product of northern wetland methane emissions based on upscaling eddy covariance observations",
author = {Peltola, Olli and
Vesala, Timo and
Gao, Yao and
R{\"a}ty, Olle and
Alekseychik, Pavel and
Aurela, Mika and
Chojnicki, Bogdan H. and
Desai, Ankur R. and
Dolman, A. J. and
Euskirchen, E. S. and
Friborg, Thomas and
G{\"o}ckede, Mathias and
Helbig, Manuel and
Humphreys, Elyn and
Jackson, Robert B. and
Jocher, Georg and
Joos, Fortunat and
Klatt, Janina and
Knox, Sara and
Kowalska, Natalia and
Kutzbach, Lars and
Lienert, Sebastian and
Lohila, Annalea and
Mammarella, Ivan and
Nadeau, Daniel F. and
Nilsson, Mats B. and
Oechel, Walter C. and
Peichl, Matthias and
Pypker, Thomas G. and
Quinton, W. L. and
Rinne, Janne and
Sachs, Torsten and
Samson, Mateusz and
Schmid, Hans Peter and
Sonnentag, Oliver and
Wille, Christian and
Zona, Donatella and
Aalto, Tuula},
journal = "Earth System Science Data, Volume 11, Issue 3",
volume = "11",
number = "3",
year = "2019",
publisher = "Copernicus GmbH",
url = "https://gwf-uwaterloo.github.io/gwf-publications/G19-140001",
doi = "10.5194/essd-11-1263-2019",
pages = "1263--1289",
abstract = "Abstract. Natural wetlands constitute the largest and most uncertain source of methane (CH4) to the atmosphere and a large fraction of them are found in the northern latitudes. These emissions are typically estimated using process ({``}bottom-up{''}) or inversion ({``}top-down{''}) models. However, estimates from these two types of models are not independent of each other since the top-down estimates usually rely on the a priori estimation of these emissions obtained with process models. Hence, independent spatially explicit validation data are needed. Here we utilize a random forest (RF) machine-learning technique to upscale CH4 eddy covariance flux measurements from 25 sites to estimate CH4 wetland emissions from the northern latitudes (north of 45∘ N). Eddy covariance data from 2005 to 2016 are used for model development. The model is then used to predict emissions during 2013 and 2014. The predictive performance of the RF model is evaluated using a leave-one-site-out cross-validation scheme. The performance (Nash{--}Sutcliffe model efficiency =0.47) is comparable to previous studies upscaling net ecosystem exchange of carbon dioxide and studies comparing process model output against site-level CH4 emission data. The global distribution of wetlands is one major source of uncertainty for upscaling CH4. Thus, three wetland distribution maps are utilized in the upscaling. Depending on the wetland distribution map, the annual emissions for the northern wetlands yield 32 (22.3{--}41.2, 95 {\%} confidence interval calculated from a RF model ensemble), 31 (21.4{--}39.9) or 38 (25.9{--}49.5) Tg(CH4) yr−1. To further evaluate the uncertainties of the upscaled CH4 flux data products we also compared them against output from two process models (LPX-Bern and WetCHARTs), and methodological issues related to CH4 flux upscaling are discussed. The monthly upscaled CH4 flux data products are available at https://doi.org/10.5281/zenodo.2560163 (Peltola et al., 2019).",
}
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<abstract>Abstract. Natural wetlands constitute the largest and most uncertain source of methane (CH4) to the atmosphere and a large fraction of them are found in the northern latitudes. These emissions are typically estimated using process (“bottom-up”) or inversion (“top-down”) models. However, estimates from these two types of models are not independent of each other since the top-down estimates usually rely on the a priori estimation of these emissions obtained with process models. Hence, independent spatially explicit validation data are needed. Here we utilize a random forest (RF) machine-learning technique to upscale CH4 eddy covariance flux measurements from 25 sites to estimate CH4 wetland emissions from the northern latitudes (north of 45∘ N). Eddy covariance data from 2005 to 2016 are used for model development. The model is then used to predict emissions during 2013 and 2014. The predictive performance of the RF model is evaluated using a leave-one-site-out cross-validation scheme. The performance (Nash–Sutcliffe model efficiency =0.47) is comparable to previous studies upscaling net ecosystem exchange of carbon dioxide and studies comparing process model output against site-level CH4 emission data. The global distribution of wetlands is one major source of uncertainty for upscaling CH4. Thus, three wetland distribution maps are utilized in the upscaling. Depending on the wetland distribution map, the annual emissions for the northern wetlands yield 32 (22.3–41.2, 95 % confidence interval calculated from a RF model ensemble), 31 (21.4–39.9) or 38 (25.9–49.5) Tg(CH4) yr−1. To further evaluate the uncertainties of the upscaled CH4 flux data products we also compared them against output from two process models (LPX-Bern and WetCHARTs), and methodological issues related to CH4 flux upscaling are discussed. The monthly upscaled CH4 flux data products are available at https://doi.org/10.5281/zenodo.2560163 (Peltola et al., 2019).</abstract>
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%0 Journal Article %T Monthly gridded data product of northern wetland methane emissions based on upscaling eddy covariance observations %A Peltola, Olli %A Vesala, Timo %A Gao, Yao %A Räty, Olle %A Alekseychik, Pavel %A Aurela, Mika %A Chojnicki, Bogdan H. %A Desai, Ankur R. %A Dolman, A. J. %A Euskirchen, E. S. %A Friborg, Thomas %A Göckede, Mathias %A Helbig, Manuel %A Humphreys, Elyn %A Jackson, Robert B. %A Jocher, Georg %A Joos, Fortunat %A Klatt, Janina %A Knox, Sara %A Kowalska, Natalia %A Kutzbach, Lars %A Lienert, Sebastian %A Lohila, Annalea %A Mammarella, Ivan %A Nadeau, Daniel F. %A Nilsson, Mats B. %A Oechel, Walter C. %A Peichl, Matthias %A Pypker, Thomas G. %A Quinton, W. L. %A Rinne, Janne %A Sachs, Torsten %A Samson, Mateusz %A Schmid, Hans Peter %A Sonnentag, Oliver %A Wille, Christian %A Zona, Donatella %A Aalto, Tuula %J Earth System Science Data, Volume 11, Issue 3 %D 2019 %V 11 %N 3 %I Copernicus GmbH %F Peltola-2019-Monthly %X Abstract. Natural wetlands constitute the largest and most uncertain source of methane (CH4) to the atmosphere and a large fraction of them are found in the northern latitudes. These emissions are typically estimated using process (“bottom-up”) or inversion (“top-down”) models. However, estimates from these two types of models are not independent of each other since the top-down estimates usually rely on the a priori estimation of these emissions obtained with process models. Hence, independent spatially explicit validation data are needed. Here we utilize a random forest (RF) machine-learning technique to upscale CH4 eddy covariance flux measurements from 25 sites to estimate CH4 wetland emissions from the northern latitudes (north of 45∘ N). Eddy covariance data from 2005 to 2016 are used for model development. The model is then used to predict emissions during 2013 and 2014. The predictive performance of the RF model is evaluated using a leave-one-site-out cross-validation scheme. The performance (Nash–Sutcliffe model efficiency =0.47) is comparable to previous studies upscaling net ecosystem exchange of carbon dioxide and studies comparing process model output against site-level CH4 emission data. The global distribution of wetlands is one major source of uncertainty for upscaling CH4. Thus, three wetland distribution maps are utilized in the upscaling. Depending on the wetland distribution map, the annual emissions for the northern wetlands yield 32 (22.3–41.2, 95 % confidence interval calculated from a RF model ensemble), 31 (21.4–39.9) or 38 (25.9–49.5) Tg(CH4) yr−1. To further evaluate the uncertainties of the upscaled CH4 flux data products we also compared them against output from two process models (LPX-Bern and WetCHARTs), and methodological issues related to CH4 flux upscaling are discussed. The monthly upscaled CH4 flux data products are available at https://doi.org/10.5281/zenodo.2560163 (Peltola et al., 2019). %R 10.5194/essd-11-1263-2019 %U https://gwf-uwaterloo.github.io/gwf-publications/G19-140001 %U https://doi.org/10.5194/essd-11-1263-2019 %P 1263-1289
Markdown (Informal)
[Monthly gridded data product of northern wetland methane emissions based on upscaling eddy covariance observations](https://gwf-uwaterloo.github.io/gwf-publications/G19-140001) (Peltola et al., GWF 2019)
- Monthly gridded data product of northern wetland methane emissions based on upscaling eddy covariance observations (Peltola et al., GWF 2019)
ACL
- Olli Peltola, Timo Vesala, Yao Gao, Olle Räty, Pavel Alekseychik, Mika Aurela, Bogdan H. Chojnicki, Ankur R. Desai, A. J. Dolman, E. S. Euskirchen, Thomas Friborg, Mathias Göckede, Manuel Helbig, Elyn Humphreys, Robert B. Jackson, Georg Jocher, Fortunat Joos, Janina Klatt, Sara Knox, et al.. 2019. Monthly gridded data product of northern wetland methane emissions based on upscaling eddy covariance observations. Earth System Science Data, Volume 11, Issue 3, 11(3):1263–1289.