Context. Total and spectral solar irradiance are key parameters in the assessment of solar influence on changes in the Earth's climate. Aims. We present a SATIRE-S reconstruction of daily solar irradiance spanning 1974 to 2013, based on full-disc observations from the KPVT, SoHO/MDI and SDO/HMI. Methods. SATIRE-S ascribes variation in solar irradiance, on timescales greater than a day, to photospheric magnetism. The solar spectrum is reconstructed from the apparent surface coverage of bright magnetic features and sunspots in the daily data using the modelled intensity spectra of these magnetic structures. We cross-calibrated the various data sets, harmonizing the model input so to yield a single consistent time series as the output.Results. The model replicates 92% (R = 0.957) of the variability, and the secular decline between the 1996 and 2008 solar cycle minima in the PMOD TSI composite. The model also reproduced most of the variability in solar Lyman-α irradiance and the Mg II index. The ultraviolet solar irradiance measurements from the UARS and SORCE missions exhibit discrepant solar cycle variation, especially above 240 nm. As a result, the model while able to replicate the rotational variability in these records, aligned with certain observations better than others in terms of the long-term trends. The solar cycle variation in the ultraviolet in the reconstruction is confirmed by the close match to that in a SUSIMbased empirical model from a previous study. As with earlier similar investigations, the reconstruction cannot reproduce the long-term trends in SORCE/SIM spectrometry. We argue, from the apparent lack of solar cycle modulation in SIM SSI and the dissimilarity * The contents of this chapter are identical to the submitted version of Yeo,