The energy we receive
Total solar irradiance is the energy received at the top of the atmosphere, about 1,361 W/m². It varies by only about 0.1 % over the cycle; sunspots lower it, faculae raise it.
Illustrative surface and corona; spots from the latest monthly sunspot number.
Show the data as a table
Show the data as a table
NRLTSI2 is the model of the NOAA “solar irradiance” Climate Data Record: irradiance is reconstructed from sunspot darkening and facular brightening, calibrated against the satellite measurements (SORCE/TIM) available since 1978 (Coddington et al., 2016). Unit: W/m² at 1 astronomical unit.
Values before 17 November 1978 (start of continuous measurements) are flagged “estimated”; the model uncertainty is imported with each value.
- NRLTSI2 daily total solar irradiance (NOAA CDR via LASP LISIRD)
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Coddington, O., Lean, J. L., Pilewskie, P., Snow, M., & Lindholm, D. (2016). A Solar Irradiance Climate Data Record. Bulletin of the American Meteorological Society, 97, 1265–1282. Data: NRLTSI2 via LASP LISIRD.
· doi:10.1175/BAMS-D-14-00265.1 · source page ↗
Licence : NOAA Climate Data Record, public domain; cite Coddington et al. (2016) · retrieved on Oct 23, 2026 · SHA-256 f6ca2f1a23d4…