Simultaneous shipborne measurements of CO<sub>2</sub>, CH<sub>4</sub> and CO and their application to improving greenhouse-gas flux estimates in Australia
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Published:2019-05-24
Issue:10
Volume:19
Page:7055-7072
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ISSN:1680-7324
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Container-title:Atmospheric Chemistry and Physics
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language:en
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Short-container-title:Atmos. Chem. Phys.
Author:
Bukosa Beata, Deutscher Nicholas M.ORCID, Fisher Jenny A.ORCID, Kubistin Dagmar, Paton-Walsh ClareORCID, Griffith David W. T.ORCID
Abstract
Abstract. Quantitative understanding of the sources and sinks of greenhouse
gases is essential for predicting greenhouse-gas–climate feedback processes
and their impacts on climate variability and change. Australia plays a
significant role in driving variability in global carbon cycling, but the
budgets of carbon gases in Australia remain highly uncertain. Here, shipborne
Fourier transform infrared spectrometer measurements collected around
Australia are used together with a global chemical transport model
(GEOS-Chem) to analyse the variability of three direct and indirect carbon
greenhouse gases: carbon dioxide (CO2), methane (CH4) and
carbon monoxide (CO). Using these measurements, we provide an updated
distribution of these gases. From the model, we quantify their sources and
sinks, and we exploit the benefits of multi-species analysis to explore
co-variations to constrain relevant processes. We find that for all three
gases, the eastern Australian coast is largely influenced by local anthropogenic
sources, while the southern, western and northern coasts are characterised by a mixture
of anthropogenic and natural sources. Comparing coincident and co-located
enhancements in the three carbon gases highlighted several common sources
from the Australian continent. We found evidence for 17 events with similar
enhancement patterns indicative of co-emission and calculated enhancement
ratios and modelled source contributions for each event. We found that
anthropogenic co-enhancement events are common along the eastern coast, while
co-enhancement events in the tropics primarily derive from biomass burning
sources. While the GEOS-Chem model generally reproduced the timing of
co-enhancement events, it was less able to reproduce the magnitude of
enhancements. We used these differences to identify underestimated,
overestimated and missing processes in the model. We found model
overestimates of CH4 from coal burning and underestimates of all
three gases from biomass burning. We identified missing sources from fossil
fuel, biofuel, oil, gas, coal, livestock, biomass burning and the biosphere
in the model, pointing to the need to further develop and evaluate greenhouse-gas emission inventories for the Australian continent.
Funder
University of Wollongong Australian Research Council
Publisher
Copernicus GmbH
Subject
Atmospheric Science
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