Article information

2026 , Volume 31, ¹ 1, p.23-38

Fedorov V.M., Kostin A.A.

The calculation of the Earths surface irradiation characteristics for the 9999 BC - AD 9998

Context. The irradiation characteristics for the Earth’s surface and its latitudinal zones in tropical years and their parts can be precisely calculated based on NASA ephemerides, by accepting the Earth’s ellipsoidal form. Due to ephemerides, the long-term changes and short-term disturbances of the Earth’s orbital movement and rotation, caused by the Solar system bodies, are considered. The Earth’s atmosphere, relief, and tide deformations are not taken into account. The solar radiance intensity is assumed to be constant.

The main irradiation characteristics are: IrE — energy (J); IrSE — specific energy (J/m2); and IrI — intensity (W/m2). For previous calculations, the DE406 ephemerides were used by the authors. They formed the set of IrE for all 5-degrees latitudinal zones and all tropical months in the range of 3000 BC — AD 2999.

Purpose. The aim of this work is the revision of the calculation method: the use of DE441 ephemerides with extended time range; the division of the Earth’s surface into 1-degree latitudinal zones, and the tropical years up to tropical days; and additional calculations of IrSE and IrI.

Methodology. The precise and approximate formulas for calculations, description of the work stages and calculation errors are presented.

Findings. The authors conducted precise calculations of the irradiation characteristics for the surface and latitudinal zones of the Earth in tropical years and their parts for the interval of 9999 BC — AD 9998, with dating and durations of tropical years and their parts.

Value. The data can be used in irradiation blocks of physical-mathematical and neural network models of weather and climate.

[link to elibrary.ru]

Keywords: irradiation characteristics, latitudinal zones, tropical years

doi: 10.25743/ICT.2026.31.1.003

Author(s):
Fedorov Valeriy Michailovich
PhD.
Position: Leading research officer
Office: Lomonosov Moscow State University
Address: 119991, Russia, Moscow, 1, Leninskie Gory
Phone Office: (495) 939 1763
E-mail: fedorov.msu@mail.ru
SPIN-code: 1550-3433

Kostin Andrey Anatolievich
Position: engineer
Office: Lomonosov Moscow State University
Address: 119991, Russia, Moscow, 1, Leninskie Gory
Phone Office: (495) 412 3014
E-mail: ank_@bk.ru

References:
1. Milankovich M. Theorie mathematique des phenomenes thermique produits par la radiation solaire. Paris: Gauthier–Villars; 1920: 399.

2. Sharaf Sh.G., Budnikova N.A. On the Earth’s orbital elements age-old changes affecting the geological past climates. The Bulletin of Theoretical Astronomy Institute of the USSR Academy of Sciences. 1967; 11(4):231–261. (In Russ.)

3. Vernekar A. Long-period global variations of incoming solar radiation. Meteorological Monographs. American Meteorological Society; 1972; 12(34):107.

4. Berger A. Long-term variation of caloric insolation resulting from the Earth’s orbital elements. Quaternary Research. 1978; (9):139–167.

5. Laskar J., Joutel F., Boudin F. Orbital, precessional and insolation quantities for the Earth from -20 Myr to +10 Myr. Astronomy and Astrophysics. 1993; (287):522–533.

6. Borisenkov Å.Đ., Tsvetkov A.V., Agaponov S.V. On some characteristics of insolation changes in the past and the future. Climatic Change. 1983; (5):237–244.

7 . Loutre M.F., Berger A., Bretagnon E., Blanc P-L. Astronomical frequencies for climate research at the decadal to century time scale. Climate Dynamics. 1992; (7):181–194.

8. Bertrand C., Loutre M.F., Berger A. High frequency variations of the Earth’s orbital parameters and climate change. Geophysical Research Letters. 2002; 29(18):40-1–40-3. DOI:10.1029/2002GL015622.

9. Berger A., Loutre M.F., Yin Q. Total irradiation during any time interval of the year using elliptic integrals. Quaternary Science Reviews. 2010; (29):1968–1982. DOI:10.1016/j.quascirev.2010.05.07.14.

10. Cionco R.G., Soon W.W-H. Short-term orbital forcing: a quasi-review and a reappraisal of realistic boundary conditions for climate modeling. Earth-Science Reviews. 2017; (166):206–222.

11. Fedorov V.M., Kostin A.A. The calculation of the Earth’s insolation for the 3000 BC AD 2999. Springer Geology. 2020; (1):181–192. DOI:10.1007/978-3-030-38177-6_20.

12. Fedorov V.M., Kostin A.A., Frolov D.M. Influence of the shape of the Earth on the characteristics of the irradiation of the Earth. Izvestiya — Atmospheric and Oceanic Physics. 2020; 56(10):1301–1313. DOI:10.1134/S0001433820100035.

13. Fedorov V.M. Problems of parameterization of the radiation block in physical and mathematical climate models and the possibility of their solution. Physics Uspekhi. 2023; 66(9):914–930. DOI:10.3367/UFNe.2023.03.039339.

14. Crucifix M. Palinsol: R package to compute incoming solar radiation (insolation) for paleoclimate studies. Available at: https://zenodo.org/records/14893715 (accessed on May 5, 2025).

15. Oliveira E.D. Daily INSOLation (DINSOL-v1.0): an intuitive tool for classrooms and specifying solar radiation boundary conditions. Geoscientific Model Development. 2023; (16):2371–2390. DOI:10.5194/gmd-16-2371-2023.

16. Kopp G., Lean J. A new lower value of total solar irradiance: evidence and climate significance. Geophysical Research Letters. 2011; (37):L01706. DOI:10.1029/2010GL045777.

Bibliography link:
Fedorov V.M., Kostin A.A. The calculation of the Earths surface irradiation characteristics for the 9999 BC - AD 9998 // Computational technologies. 2026. V. 31. ¹ 1. P. 23-38
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