Abstract

Abstract. Atmospheric inverse modelling has the potential to provide observation-based estimates of greenhouse gas emissions at the country scale, thereby allowing for an independent validation of national emission inventories. Here, we present a regional-scale inverse modelling study to quantify the emissions of methane (CH4) from Switzerland, making use of the newly established CarboCount-CH measurement network and a high-resolution Lagrangian transport model. In our reference inversion, prior emissions were taken from the "bottom-up" Swiss Greenhouse Gas Inventory (SGHGI) as published by the Swiss Federal Office for the Environment in 2014 for the year 2012. Overall we estimate national CH4 emissions to be 196 ± 18 Gg yr−1 for the year 2013 (1σ uncertainty). This result is in close agreement with the recently revised SGHGI estimate of 206 ± 33 Gg yr−1 as reported in 2015 for the year 2012. Results from sensitivity inversions using alternative prior emissions, uncertainty covariance settings, large-scale background mole fractions, two different inverse algorithms (Bayesian and extended Kalman filter), and two different transport models confirm the robustness and independent character of our estimate. According to the latest SGHGI estimate the main CH4 source categories in Switzerland are agriculture (78 %), waste handling (15 %) and natural gas distribution and combustion (6 %). The spatial distribution and seasonal variability of our posterior emissions suggest an overestimation of agricultural CH4 emissions by 10 to 20 % in the most recent SGHGI, which is likely due to an overestimation of emissions from manure handling. Urban areas do not appear as emission hotspots in our posterior results, suggesting that leakages from natural gas distribution are only a minor source of CH4 in Switzerland. This is consistent with rather low emissions of 8.4 Gg yr−1 reported by the SGHGI but inconsistent with the much higher value of 32 Gg yr−1 implied by the EDGARv4.2 inventory for this sector. Increased CH4 emissions (up to 30 % compared to the prior) were deduced for the north-eastern parts of Switzerland. This feature was common to most sensitivity inversions, which is a strong indicator that it is a real feature and not an artefact of the transport model and the inversion system. However, it was not possible to assign an unambiguous source process to the region. The observations of the CarboCount-CH network provided invaluable and independent information for the validation of the national bottom-up inventory. Similar systems need to be sustained to provide independent monitoring of future climate agreements.

Highlights

  • Atmospheric methane (CH4) acts as an important greenhouse gas (GHG) whose man-made increase from pre-industrial to present-day levels directly and indirectly contributes 0.97 (0.74–1.20) W m−2 to present-day global radiative forcing (Myhre et al, 2013)

  • The maximum likelihood (ML) method applied as an alternative is an objective method to tune the free parameters of an inversion, but this does not necessarily correspond to the best set-up since it cannot account for potential biases arising from transport errors or the problem in representing the release height of the particles

  • Average source sensitivities as calculated with FLEXPARTCOSMO on the reduced grid are shown in Fig. 1 for the base inversion as the combined sensitivity of the four sites BEO, Lägern Hochwacht (LHW), sites ranged between 16.2 nmol mol−1 (SSL), and JFJ

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Summary

Introduction

Atmospheric methane (CH4) acts as an important greenhouse gas (GHG) whose man-made increase from pre-industrial to present-day levels (from ≈ 700 nmol mol−1 in 1750 to 1819 nmol mol−1 in 2012) directly and indirectly contributes 0.97 (0.74–1.20) W m−2 to present-day global radiative forcing (Myhre et al, 2013). Natural sources (wetlands, lakes, geological seeps, termites, methane hydrates, and wild animals) and anthropogenic sources (fossil fuel extraction, distribution and combustion, rice cultivation, ruminants, and waste) each contribute about half to CH4 emissions to the atmosphere (Kirschke et al, 2013), but larger uncertainties are connected with the natural sources. Owing to its comparatively short atmospheric lifetime (≈ 10 years), CH4 has been classified as a short-lived climate pollutant, and reducing anthropogenic CH4 emissions has become a promising target to lower nearterm radiative forcing (Ramanathan and Xu, 2010; Shindell et al, 2012). The Kyoto Protocol sets legally binding GHG emission reduction targets for Annex I countries and the United Nations Framework Convention on Climate Change (UNFCCC) calls signatory countries to report their annual GHG emissions of CO2, CH4, nitrous oxide, sulfur hexafluoride, and halocarbons

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