Articles | Volume 24, issue 6
https://doi.org/10.5194/acp-24-3613-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/acp-24-3613-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Quantifying the tropospheric ozone radiative effect and its temporal evolution in the satellite era
Richard J. Pope
CORRESPONDING AUTHOR
School of Earth and Environment, University of Leeds, Leeds, UK
National Centre for Earth Observation, University of Leeds, Leeds, UK
Alexandru Rap
School of Earth and Environment, University of Leeds, Leeds, UK
Matilda A. Pimlott
School of Earth and Environment, University of Leeds, Leeds, UK
Brice Barret
Laboratoire d'Aérologie (LAERO), Université Toulouse III – Paul Sabatier, CNRS, Toulouse, France
Eric Le Flochmoen
Laboratoire d'Aérologie (LAERO), Université Toulouse III – Paul Sabatier, CNRS, Toulouse, France
Brian J. Kerridge
Remote Sensing Group, STFC Rutherford Appleton Laboratory, Chilton, UK
National Centre for Earth Observation, STFC Rutherford Appleton Laboratory, Chilton, UK
Richard Siddans
Remote Sensing Group, STFC Rutherford Appleton Laboratory, Chilton, UK
National Centre for Earth Observation, STFC Rutherford Appleton Laboratory, Chilton, UK
Barry G. Latter
Remote Sensing Group, STFC Rutherford Appleton Laboratory, Chilton, UK
National Centre for Earth Observation, STFC Rutherford Appleton Laboratory, Chilton, UK
Lucy J. Ventress
Remote Sensing Group, STFC Rutherford Appleton Laboratory, Chilton, UK
National Centre for Earth Observation, STFC Rutherford Appleton Laboratory, Chilton, UK
Anne Boynard
LATMOS/IPSL, Sorbonne Université, UVSQ, CNRS, Paris, 75005, France
SPASCIA, Ramonville-Saint-Agne, 31520, France
Christian Retscher
ESA/ESRIN, Frascati, Italy
Wuhu Feng
School of Earth and Environment, University of Leeds, Leeds, UK
National Centre for Atmospheric Science, University of Leeds, Leeds, UK
Richard Rigby
School of Earth and Environment, University of Leeds, Leeds, UK
Centre for Environmental Modelling and Computation, University of Leeds, Leeds, UK
Sandip S. Dhomse
School of Earth and Environment, University of Leeds, Leeds, UK
National Centre for Earth Observation, University of Leeds, Leeds, UK
Catherine Wespes
Spectroscopy, Quantum Chemistry and Atmospheric Remote Sensing, Université libre de Bruxelles (ULB), Brussels, Belgium
Martyn P. Chipperfield
School of Earth and Environment, University of Leeds, Leeds, UK
National Centre for Earth Observation, University of Leeds, Leeds, UK
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Cited
3 citations as recorded by crossref.
- Investigation of the impact of satellite vertical sensitivity on long-term retrieved lower-tropospheric ozone trends R. Pope et al. 10.5194/acp-24-9177-2024
- Observation-Based Ozone Formation Rules by Gradient Boosting Decision Trees Model in Typical Chemical Industrial Parks N. Cheng et al. 10.3390/atmos15050600
- WRF-Chem Modeling of Tropospheric Ozone in the Coastal Cities of the Gulf of Finland G. Nerobelov et al. 10.3390/atmos15070775
3 citations as recorded by crossref.
- Investigation of the impact of satellite vertical sensitivity on long-term retrieved lower-tropospheric ozone trends R. Pope et al. 10.5194/acp-24-9177-2024
- Observation-Based Ozone Formation Rules by Gradient Boosting Decision Trees Model in Typical Chemical Industrial Parks N. Cheng et al. 10.3390/atmos15050600
- WRF-Chem Modeling of Tropospheric Ozone in the Coastal Cities of the Gulf of Finland G. Nerobelov et al. 10.3390/atmos15070775
Latest update: 20 Nov 2024
Short summary
Tropospheric ozone is an important short-lived climate forcer which influences the incoming solar short-wave radiation and the outgoing long-wave radiation in the atmosphere (8–15 km) where the balance between the two yields a net positive (i.e. warming) effect at the surface. Overall, we find that the tropospheric ozone radiative effect ranges between 1.21 and 1.26 W m−2 with a negligible trend (2008–2017), suggesting that tropospheric ozone influences on climate have remained stable with time.
Tropospheric ozone is an important short-lived climate forcer which influences the incoming...
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