Attribution of Chemistry-Climate Model Initiative (CCMI) ozone radiative flux bias from satellites

The top-of-atmosphere (TOA) outgoing longwave flux over the 9.6 mu m ozone band is a fundamental quantity for understanding chemistry-climate coupling. However, observed TOA fluxes are hard to estimate as they exhibit considerable variability in space and time that depends on the distributions of clouds, ozone (O-3), water vapor (H2O), air temperature (T-a), and surface temperature (T-s). Benchmarking present-day fluxes and quantifying the relative influence of their drivers is the first step for estimating climate feedbacks from ozone radiative forcing and predicting radiative forcing evolution.

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Author Kuai, L.
Bowman, K. W.
Miyazaki, K.
Deushi, M.
Revell, L.
Rozanov, E.
Paulot, F.
Strode, S.
Conley, Andrew J.
Lamarque, Jean-François
Jöckel, P.
Plummer, D. A.
Oman, L. D.
Worden, Helen M.
Kulawik, S.
Paynter, D.
Stenke, A.
Kunze, M.
Publisher UCAR/NCAR - Library
Publication Date 2020-01-08T00:00:00
Digital Object Identifier (DOI) Not Assigned
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Resource Version N/A
Topic Category geoscientificInformation
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Metadata Date 2025-07-11T19:22:21.480361
Metadata Record Identifier edu.ucar.opensky::articles:23073
Metadata Language eng; USA
Suggested Citation Kuai, L., Bowman, K. W., Miyazaki, K., Deushi, M., Revell, L., Rozanov, E., Paulot, F., Strode, S., Conley, Andrew J., Lamarque, Jean-François, Jöckel, P., Plummer, D. A., Oman, L. D., Worden, Helen M., Kulawik, S., Paynter, D., Stenke, A., Kunze, M.. (2020). Attribution of Chemistry-Climate Model Initiative (CCMI) ozone radiative flux bias from satellites. UCAR/NCAR - Library. https://n2t.org/ark:/85065/d72r3vv1. Accessed 30 July 2025.

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