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Information on the International System of Units (SI) and solar constants, as published by Princeton University Press. It includes references to various studies and sources, such as the Bureau International des Poids et Mesures and Allen’s Astrophysical Quantities. The document emphasizes the importance of using exact nominal values for solar properties and conversion constants when expressing stellar properties.
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(Proposed by the Executive Committee)
Proposed by IAU Inter-Division A-G Working Group on Nominal Units for Stellar &
Planetary Astronomy
The XXIXth International Astronomical Union General Assembly,
Noting
defining the zero point for the bolometric magnitude scale (Andersen 1999), but that the resolution never subsequently reached the stage of approval by the IAU General Assembly, and was only sporadically adopted within the astronomical community,
and hence the apparent bolometric magnitude mBol for an irradiance f (in W m−^2 ) is
mBol = − 2 .5 log ( f / f◦) = − 2 .5 log f − 18 .997 351 ... (4)
The irradiance f◦ corresponds to that measured from an isotropically emit- ting radiation source with absolute bolometric magnitude MBol = 0 mag (luminosity L◦) at the standard distance^4 of 10 parsecs (based on the IAU 2012 definition of the astronomical unit).
The adopted value of f◦ agrees with some in common use (e.g., Lang 1974, Cox 2000) at the level of < 0. 1 %. Using this zero point, the nominal total solar irradiance S N^ (1361 W m−^2 ) corresponds to a solar apparent
bolometric magnitude of mBol ' − 26. 832 mag.
References
Andersen, J. 1999, Transactions of the International Astronomical Union, Series B, 23, pgs. 141 & 182
Bessell, M. S., Castelli, F., & Plez, B. 1998, Astronomy & Astrophysics, 333, 231
Binney, J., & Tremaine, S. 2008, Galactic Dynamics: Second Edition, ISBN 978-0-691-13026-2 (HB). Published by Princeton University Press, Princeton, NJ USA
Bureau International des Poids et Mesures, 2006, The International System of Units (SI), 8th edition, Organisation Intergouvernementale de la Convention du M´etre
Cox, A. N. 2000, Allen’s Astrophysical Quantities, 4th Edition
Kopp, G. 2014, Journal of Space Weather and Space Climate, 4, A
Kopp, G., Lawrence, G., Rottman, G., 2005, Solar Physics, 230, 129
Kopp, G., & Lean, J. L. 2011, Geophysical Research Letters, 38, L
Lang, K. R. 1974, Astrophysical Formulae, A Compendium for the Physicist and Astrophysicist, Springer-Verlag
Meftah, M., Irbah, A., Hauchecorne, A., et al. 2015, Solar Physics, 290, 673
Schmutz W., Fehlmann A., Finsterle W., et al. 2013, AIP Conf. Proc. 1531, p. 624627, doi:10.1063/1.
Torres, G. 2010, Astronomical Journal, 140, 1158
Wilkins, G. A. 1989, “The IAU Style Manual (1989): The Preparation of Astro- nomical Papers and Reports”
Willson, R. C. 2014, Astrophysics & Space Science, 352, 341
Notes
(^1) The notation of Mbol referring to absolute bolometric magnitude and mbol referring to appar- ent bolometric magnitude was adopted by Commission 3 (Notations) at the VIth IAU General As- sembly in Stockholm in 1938: https://www.iau.org/static/resolutions/IAU1938 French.pdf. MBol and mBol refer specifically to bolometric magnitudes defined using the zero points of this resolu- tion. (^2) Modern spaceborne total solar irradiance (TSI) instruments are absolutely calibrated at the
0.03% level (Kopp 2014). The TIM/SORCE experiment established a lower TSI value than pre- viously reported based on the fully characterized TIM instrument (Kopp et al. 2005, Kopp & Lean 2011). This revised TSI scale was later confirmed by PREMOS/PICARD, the first space- borne TSI radiometer that was irradiance-calibrated in vacuum at the TSI Radiometer Facil- ity (TRF) with SI-traceability prior to launch (Schmutz et al. 2013). The DIARAD/PREMOS (Meftah et al. 2015), ACRIM3/ACRIMSat (Willson 2014), VIRGO/SoHO, and TCTE/STP-Sat (http://lasp.colorado.edu/home/tcte/) flight instruments are now consistent with this new TSI scale within instrument uncertainties, with the DIARAD, ACRIM3, and VIRGO having made post- launch corrections and the TCTE having been validated on the TRF prior to its 2013 launch. The cycle 23 observations with these experiments are consistent with a TSI value (rounded to an appro- priate number of significant digits) and uncertainty of: S = 1361 (± 1) W m−^2 (2σ uncertainty). The uncertainty range includes contributions from the absolute accuracies of the latest TSI instru- ments as well as uncertainties in assessing a secular trend in TSI over solar cycle 23 using older measurements. Combining this total solar irradiance value with the IAU 2012 definition of the as- tronomical unit leads to a current best estimate of the mean solar luminosity of L = 4 π (1 au)^2 S = 3.8275 (± 0.0014) × 1026 W. Based on this, a nominal solar luminosity of LN^ = 3.828 × 1026 W is adopted. Using the proposed zero point L◦, the nominal solar luminosity LN^ corresponds to bolometric magnitude MBol ' 4.739 996 ... mag — i.e., sufficiently close to 4.74 mag for any foreseeable practical purpose. (^3) The terms irradiance and heat flux density are used interchangeably, both with SI
units of W m−^2 (Wilkins 1989, Bureau International des Poids et Mesures 2006). See also https://www.iau.org/publications/proceedings rules/units/. (^4) The parsec is defined as exactly (648 000/π) au (e.g. Cox 2000, Binney & Tremaine 2008).
Using the IAU 2012 Resolution B2 definition of the astronomical unit, the parsec corresponds to 3.085 677 581 ... × 1016 m. As the absolute bolometric magnitude zero point and astronomical unit are defined exactly, further digits for the apparent bolometric magnitude zero point irradiance f◦ may be calculated if needed.
rapidly increasing accuracy of spectroscopic, photometric, and interfero- metric observations of stars and extrasolar planets^1 , and
Recommends
In all scientific publications in which accurate values of basic stellar or planetary properties are derived or quoted:
SOLAR CONVERSION CONSTANTS 1 RN^ = 6. 957 × 108 m 1 SN^ = 1361 W m−^2 1 LN^ = 3. 828 × 1026 W 1 T (^) eNff = 5772 K 1(GM)N^ = 1 .327 124 4 × 1020 m^3 s−^2
1 RN eE = 6. 3781 × 106 m 1 RN pE = 6. 3568 × 106 m 1 RN eJ = 7. 1492 × 107 m 1 RN pJ = 6. 6854 × 107 m 1 (GM)NE = 3 .986 004 × 1014 m^3 s−^2 1 (GM)NJ = 1 .266 865 3 × 1017 m^3 s−^2
Explanation
(Luzum et al. 2011), subtracting off the contribution from the Galilean satel- lites (Jacobson et al. 2000). The quoted value is rounded to the precision within which the TCB and TDB values agree, and the uncertainties in the masses of the satellites are negligible.
\newcommand{\Qnom}{\hbox{$\mathcal{Q}ˆ{\rm N}{\odot}$}} \newcommand{\Qn}{\mathcal Qˆ{\rm N}{\odot}}
References
Archinal, B. A., A’Hearn, M. F., Bowell, E., et al. 2011, Celestial Mechanics and Dynamical Astronomy 109, 101
Haberreiter, M., Schmutz, W., Kosovichev, A. G. 2008, ApJ, 675, L
Harmanec, P., Prˇsa, A. 2011, PASP, 123, 976
Jacobson, R. A., Haw, R. J., McElrath, T. P., & Antreasian, P. G. 2000, J. Astro- naut. Sci. 48(4), 495
Kopp, G. 2014, Journal of Space Weather and Space Climate, 4, A
Kopp, G., Lawrence, G., Rottman, G., 2005, Solar Physics, 230, 129
Kopp, G., & Lean, J. L. 2011, Geophys. Res. Letters, 38, L
Luzum, B., Capitaine, N., Fienga, A., et al. 2011, Celestial Mechanics and Dy- namical Astronomy, 110, 293
McCarthy, D. D. & Petit, G. 2004 IERS Technical Note No. 32, 1
Meftah, M., Irbah, A., Hauchecorne, A., et al. 2015, Solar Physics, 290, 673
Petit, G., Luzum, B. (Eds.) 2010 IERS Technical Note No. 36
Pouillet, C. S. M. 1838, Memoire sur le chaleur solaire, Paris, Bachelier
Prˇsa, A. & Harmanec, P. 2012, Proc. IAU Symp. 282, Cambridge Univ., Press, 339
Schmutz W., Fehlmann A., Finsterle W., et al. 2013, AIP Conf. Proc. 1531, p. 624627, doi:10.1063/1.
Torres, G., Andersen, J., Gim´enez, A. 2010, A&A Rev., 18, 67
Willson, R. C. 2014, Astrophysics & Space Science, 352, 341
Willson, R. C. 1978, Journal of Geophysical Research, 83, 4003
Notes
(^1) Note, e.g., that since projected rotational velocities of stars (v sin i) are measured in SI units,
the use of different values for the solar radius can lead to measurable differences in the rotational periods of giant stars (see Harmanec and Prˇsa 2011). (^2) Haberreiter et al. (2008) measured the solar photospheric radius to be 695 658 (± 140) km.
The adopted RN^ is based on this value, quoting an appropriate number of significant figures given the uncertainty, and differs slightly from the nominal solar radius tentatively proposed by Har- manec & Prˇsa (2011) and Prˇsa & Harmanec (2012). (^3) The TSI is variable at the ∼0.08% (∼1 W m− (^2) ) level and may be variable at slightly larger
amplitudes over timescales of centuries. Modern spaceborne TSI instruments are absolutely cal- ibrated at the 0.03% level (Kopp 2014). The TIM/SORCE experiment established a lower TSI value than previously reported based on the fully characterized TIM instrument (Kopp et al. 2005, Kopp & Lean 2011). This revised TSI scale was later confirmed by PREMOS/PICARD, the first spaceborne TSI radiometer that was irradiance-calibrated in vacuum at the TSI Radiometer Fa- cility (TRF) with SI-traceability prior to launch (Schmutz et al. 2013). The DIARAD/PREMOS (Meftah et al. 2015), ACRIM3/ACRIMSat (Willson 2014), VIRGO/SoHO, and TCTE/STP-Sat (http://lasp.colorado.edu/home/tcte/) flight instruments are now consistent with this new TSI scale within instrument uncertainties, with the DIARAD, ACRIM3, and VIRGO having made post- launch corrections and the TCTE having been validated on the TRF prior to its 2013 launch. The Cycle 23 observations with these experiments are consistent with a mean TSI value of S = 1361 W m−^2 (± 1 W m−^2 ; 2σ). The uncertainty range includes contributions from the ab- solute accuracies of the latest TSI instruments as well as uncertainties in assessing a secular trend in TSI over solar cycle 23 using older measurements. (^4) Resolution B2 of the XXVIII General Assembly of the IAU in 2012 defined the astronomical
unit to be a conventional unit of length equal to 149 597 870 700 m exactly. Using the current best estimate of the TSI (discussed in endnote 3), this is consistent with a current best estimate of the Sun’s mean radiative luminosity of L = 4 π (1 au)^2 S = 3.8275 (± 0.0014) × 1026 W. (^5) The CODATA 2014 value for the Stefan-Boltzmann constant is σ = 5 .670 367 (± 0 .000 013)×
10 −^8 W m−^2 K−^4. The current best estimate for the solar effective temperature is calculated to be Teff, = 5772.0 (± 0.8) K.
Resolves