Reproducing and Attributing IASI Radiance Trends with EC-Earth Climate Model Simulations
Year: 2025
Authors: Della Fera S., Fabiano F., Raspollini P., Ridolfi M., Von Hardenberg J., Cortesi U.
Autors Affiliation: Natl Res Council IFAC CNR, Inst Appl Phys, Sesto Fiorentino, Italy; Natl Res Council ISAC CNR, Inst Atmospher Sci & Climate, Bologna, Italy; Natl Res Council INO CNR, Natl Inst Opt, Sesto Fiorentino, Italy; Politecn Torino, Dept Environm Land & Infrastruct Engn, Turin, Italy.
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.
Journal/Review: JOURNAL OF CLIMATE
Volume: 38 (23) Pages from: 6943 to: 6959
More Information: The authors acknowledge CINECA and ECMWF for providing computational resources and EUMETSAT for making available the huge amount of L1c IASI data through the European Weather Cloud (EWC)service. The u-IASI was made available by its authors (see data availability statement) . Finally, this work has been carried out in the framework of the Earth-Moon-Mars (EMM) project (PNRR, Mission 4, Component 2, Investment 3.1, Project IR000038, CUPC53C22000870006) and of the MC-FORUM project (Meteo and Climate exploitation of FORUM) , funded by the Italian Space Agency from January 2024. The authors thank the three anonymous referees for their contributions to improving the clarity and content of the paper.KeyWords: Climate; Feedback; Radiation; Climate modelsDOI: 10.1175/JCLI-D-25-0034.1Citations: 1data from “WEB OF SCIENCE” (of Thomson Reuters) are update at: 2026-03-15References taken from IsiWeb of Knowledge: (subscribers only)
