XCO<sub>2</sub> in an emission hot-spot region: the COCCON Paris campaign 2015
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Published:2019-03-13
Issue:5
Volume:19
Page:3271-3285
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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:
Vogel Felix R.ORCID, Frey Matthias, Staufer Johannes, Hase Frank, Broquet Grégoire, Xueref-Remy Irène, Chevallier FrédéricORCID, Ciais Philippe, Sha Mahesh KumarORCID, Chelin Pascale, Jeseck Pascal, Janssen ChristofORCID, Té Yao, Groß Jochen, Blumenstock Thomas, Tu Qiansi, Orphal Johannes
Abstract
Abstract. Providing timely information on urban greenhouse gas (GHG) emissions and
their trends to stakeholders relies on reliable measurements of atmospheric
concentrations and the understanding of how local emissions and atmospheric
transport influence these observations. Portable Fourier transform infrared (FTIR) spectrometers were deployed at five stations
in the Paris metropolitan area to provide column-averaged
concentrations of CO2 (XCO2) during a field campaign in spring of
2015, as part of the Collaborative Carbon Column Observing Network (COCCON).
Here, we describe and analyze the variations of XCO2 observed at
different sites and how they changed over time. We find that observations
upwind and downwind of the city centre differ significantly in their
XCO2 concentrations, while the overall variability of the daily cycle
is similar, i.e. increasing during night-time with a strong decrease
(typically 2–3 ppm) during the afternoon. An atmospheric transport model framework (CHIMERE-CAMS) was used to simulate
XCO2 and predict the same behaviour seen in the observations, which
supports key findings, e.g. that even in a densely populated region like
Paris (over 12 million people), biospheric uptake of CO2 can be of
major influence on daily XCO2 variations. Despite a general offset
between modelled and observed XCO2, the model correctly predicts the
impact of the meteorological parameters (e.g. wind direction and speed) on
the concentration gradients between different stations. When analyzing local
gradients of XCO2 for upwind and downwind station pairs, those local gradients are found to
be less sensitive to changes in XCO2 boundary conditions and biogenic
fluxes within the domain and we find the model–data agreement further
improves. Our modelling framework indicates that the local XCO2
gradient between the stations is dominated by the fossil fuel CO2
signal of the Paris metropolitan area. This further highlights the potential
usefulness of XCO2 observations to help optimize future urban GHG
emission estimates.
Publisher
Copernicus GmbH
Subject
Atmospheric Science
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