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Reproducing and Attributing IASI Radiance Trends with EC-Earth Climate Model Simulations.

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Title: Reproducing and Attributing IASI Radiance Trends with EC-Earth Climate Model Simulations.
Authors: Della Fera, Stefano1 (AUTHOR) s.dellafera@ifac.cnr.it, Fabiano, Federico2 (AUTHOR), Raspollini, Piera1 (AUTHOR), Ridolfi, Marco3 (AUTHOR), von Hardenberg, Jost4 (AUTHOR), Cortesi, Ugo1 (AUTHOR)
Source: Journal of Climate. Dec2025, Vol. 38 Issue 23, p6943-6959. 17p.
Subjects: Radiance, Brightness temperature, Spectrum analysis, Climate change, Atmospheric models, Greenhouse gases, Weather
Abstract: The evolution of spectrally resolved outgoing longwave radiation measured at the top of the atmosphere (TOA) reflects the fingerprints of key geophysical variables, serving as a powerful tool for studying climate change. In this work, trends in TOA brightness temperature (BT) in the midinfrared spectral range observed by the Infrared Atmospheric Sounding Interferometer (IASI) are compared with trends in synthetic BTs generated from a set of atmosphere-only simulations with the EC-Earth3 climate model (v3.3.3), over the period 2008–19. Despite the presence of spectral biases, the model simulations effectively reproduce the IASI trends in the thermal infrared. A spectral kernel analysis is then applied to the synthetic radiances to quantify the contributions of temperature, surface temperature, water vapor, clouds, and greenhouse gases to these trends. The negative trend found in the core of the CO2 band is attributed to the stratospheric cooling, which is overestimated in the climate model simulations. In the wing of the CO2 band, the negative trend in radiance results from the combined effect of a positive contribution from the increasing tropospheric temperature and a negative contribution driven by rising atmospheric CO2 concentration. In the atmospheric windows, clouds have a negative impact on the radiance trend and also significantly affect the interannual variability of the model's radiance. Last, the near-zero trend in the water vapor band reflects a balance between the positive trend driven by temperature increases and the negative trend associated with water vapor changes. This work highlights the utility of spectrally resolved radiances to disentangle forcing and feedback processes, improving climate model evaluation. [ABSTRACT FROM AUTHOR]
Copyright of Journal of Climate is the property of American Meteorological Society and its content may not be copied or emailed to multiple sites without the copyright holder's express written permission. Additionally, content may not be used with any artificial intelligence tools or machine learning technologies. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)
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  Data: Reproducing and Attributing IASI Radiance Trends with EC-Earth Climate Model Simulations.
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  Data: <searchLink fieldCode="JN" term="%22Journal+of+Climate%22">Journal of Climate</searchLink>. Dec2025, Vol. 38 Issue 23, p6943-6959. 17p.
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  Label: Abstract
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  Data: The evolution of spectrally resolved outgoing longwave radiation measured at the top of the atmosphere (TOA) reflects the fingerprints of key geophysical variables, serving as a powerful tool for studying climate change. In this work, trends in TOA brightness temperature (BT) in the midinfrared spectral range observed by the Infrared Atmospheric Sounding Interferometer (IASI) are compared with trends in synthetic BTs generated from a set of atmosphere-only simulations with the EC-Earth3 climate model (v3.3.3), over the period 2008–19. Despite the presence of spectral biases, the model simulations effectively reproduce the IASI trends in the thermal infrared. A spectral kernel analysis is then applied to the synthetic radiances to quantify the contributions of temperature, surface temperature, water vapor, clouds, and greenhouse gases to these trends. The negative trend found in the core of the CO2 band is attributed to the stratospheric cooling, which is overestimated in the climate model simulations. In the wing of the CO2 band, the negative trend in radiance results from the combined effect of a positive contribution from the increasing tropospheric temperature and a negative contribution driven by rising atmospheric CO2 concentration. In the atmospheric windows, clouds have a negative impact on the radiance trend and also significantly affect the interannual variability of the model's radiance. Last, the near-zero trend in the water vapor band reflects a balance between the positive trend driven by temperature increases and the negative trend associated with water vapor changes. This work highlights the utility of spectrally resolved radiances to disentangle forcing and feedback processes, improving climate model evaluation. [ABSTRACT FROM AUTHOR]
– Name: AbstractSuppliedCopyright
  Label:
  Group: Ab
  Data: <i>Copyright of Journal of Climate is the property of American Meteorological Society and its content may not be copied or emailed to multiple sites without the copyright holder's express written permission. Additionally, content may not be used with any artificial intelligence tools or machine learning technologies. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract.</i> (Copyright applies to all Abstracts.)
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RecordInfo BibRecord:
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      – Type: doi
        Value: 10.1175/JCLI-D-25-0034.1
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      – Code: eng
        Text: English
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        PageCount: 17
        StartPage: 6943
    Subjects:
      – SubjectFull: Radiance
        Type: general
      – SubjectFull: Brightness temperature
        Type: general
      – SubjectFull: Spectrum analysis
        Type: general
      – SubjectFull: Climate change
        Type: general
      – SubjectFull: Atmospheric models
        Type: general
      – SubjectFull: Greenhouse gases
        Type: general
      – SubjectFull: Weather
        Type: general
    Titles:
      – TitleFull: Reproducing and Attributing IASI Radiance Trends with EC-Earth Climate Model Simulations.
        Type: main
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            NameFull: Della Fera, Stefano
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            NameFull: Fabiano, Federico
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            NameFull: Raspollini, Piera
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            NameFull: Ridolfi, Marco
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            NameFull: von Hardenberg, Jost
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            – D: 01
              M: 12
              Text: Dec2025
              Type: published
              Y: 2025
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              Value: 08948755
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              Value: 38
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              Value: 23
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