The spectral longwave feedback parameter quantifies the change in Earth's spectrally resolved outgoing longwave radiation (OLR) in response to warming. It contains the radiative signature of all longwave
This experiment contains the monthly global mean all-sky spectrally resolved outgoing longwave radiation (OLR) calculated based on model output of the MPI-ESM1-2-HR model performing the 'historical' experiment
This experiment contains the spectrally resolved surface feedback calculated based on the 1D RCE model konrad using the line-by-line radiative transfer model ARTS for surface temperatures of 268K, 278K,
This experiment contains the monthly global mean all-sky spectrally resolved outgoing longwave radiation (OLR) calculated from observations of the Infrared Atmospheric Sounding Interferometer (IASI). For
This experiment contains the monthly global mean all-sky spectrally resolved outgoing longwave radiation calculated from the 1-D radiative-convective equilibrium model konrad using the radiative transfer