Astronomical School’s Report, 2017, Volume 13, Issue 2, Pages 68–80
UDC 523.98
Sources of solar energy and interplanetary magnetic field
Krivodubskij V.N.
Astronomical Observatory of Taras Shevchenko National University of Kyiv, Observatorna str. 3, 04053 Kyiv, Ukraine
Abstract
The sources of energy of solar activity are analyzed. The primary source of solar energy is the core of the Sun, where as a result of the reactions of thermonuclear fusion, energy is released in the form of γ-quanta and neutrino particles that propagate outward. When approaching the surface due to the fall in temperature and the increase in the opacity of the substance, the fully ionized solar plasma, from certain depths, passes into the state of partial ionization. As a result, a Schwarzschild criterion of the emergence of a convective energy transfer due to hydrodynamic motions begins to run at a distance of 0.3 solar radius from the surface. Above this boundary lies a layer of convective turbulence, in which energy is transferred mainly by a moving substance, and not by radiation. It is called the convective zone. Ultimately, the part of the radiant energy transferred to the surface gives the opportunity to observe the Sun in different wavelength ranges. While the second part of the upward energy, which is due to convective motions, will manifest itself at the photospheric level in the form of granulation movements of various scales accessible for observation. However, part of the flow of energy coming from the interior of the Sun, accumulates and is carried upwards in the “magnetic form”. An important specific property of this highly effective mechanism of magnetic energy transfer is its significant variations in time, which are manifested in cyclic changes of the majority of phenomena generated by magnetic fields, called solar activity. The specificity of this energy transfer is manifested in the non-stationary flare conversion of magnetic energy into heat, as well as in the kinetic energy of accelerated particles and macroscopic (coronal) plasma emissions. The role of the landfill, where the main processes responsible for cyclic manifestations of solar activity originate, is played by the convective zone. In the depths of the convective zone, as a result of the dynamo mechanism, some of the kinetic energy of the hydrodynamic motions (differential rotation and gyrotropic turbulent convection) is converted into magnetic energy during the solar cycle, thereby strengthening the weak magnetic field of the Sun of relic origin. The global magnetic field generated in depths is transferred to the solar surface due to its magnetic buoyancy. Surface magnetic structures change the state of the Sun's atmosphere, cause an irregular part of the radiation and serve as a source of powerful non-stationary phenomena in the outer atmospheric layers (photosphere, chromosphere and corona). The modern concept of such phenomena as hot solar corona, solar wind and interplanetary magnetic field that form space weather in the interplanetary space is reviewed. The contribution of the “Kiev coronal school” of Vsekhsviatskij S.K. to the development of the concept of the dynamic corona of the Sun is noted.
Keywords: Sun; radiation; convection; magnetic energy; space weather; corona; solar wind; interplanetary magnetic fields
References
- Vandakurov Yu.V. (1976). Konvektsiya na Solntse i 11-letny tsikl. M.: Nauka. 156 p.
- Priest E.R. Solar Magnetohydrodynamics. Dordrecct–Boston–London: D.Reidel Publishing Company, 1981.
- Solov’ev A.A., Kirichek E.A. (2004). Diffuznaya teoriya solnechnogo magnitnogo tsikla. Elista–S.Peterburg: Izdatel’stvo Kalmytskogo GU. 181 p.
- Miesch M.S. (2005). Large-scale dynamics of the convection zone and tachocline. Living Rev. Solar Phys., 2, No. 1, 1–139. https://doi.org/10.12942/lrsp-2005-1
- Filippov B.P. (2007). Eruptivnye protsessy na Solntse. M.: Fizmatlit. 216 p.
- Hathaway D.H. (2015). The solar cycle. Living Rev. Solar Phys., 12, No. 4, 1–87. https://doi.org/10.1007/lrsp-2015-4
- Vaynshteyn S.I., Zel’dovich Ya.B., Ruzmaykin A.A. (1980). Turbulentnoe dinamo v astrofizike. M.: Nauka. 352 p.
- Zeldovich Ya.B., Ruzmaikin A.A., Sokoloff D.D. Magnetic Fields in Astrophysics. New York: Gordon and Breach, 1983.
- Krause F., Rädler K.-H. (1980). Mean Field Magnetohydrodynamics and Dynamo Theory. Oxford: Pergamon Press, Ltd.. 271 p.
- Krivodubskij V.N. (1998). Rotational anisotropy and magnetic quenching of gyrotropic turbulence in the solar convective zone. Astron. Reports., 42, 122–126.
- Krivodubskij V.N. (2001). The structure of the global solar magnetic field excited by the turbulent dynamo mechanism. Astron. Reports., 45, 738–745. https://doi.org/10.1134/1.1398923
- Krivodubskij V.N. (2005). Turbulent dynamo near tachocline and reconstruction of azimuthal magnetic field in the solar convection zone. Astron. Nachrichten., 326, No. 1, 61–74. https://doi.org/10.1002/asna.200310340
- Krivodubskij V.N. (2015). Small scale alpha-squared effect in the solar convection zone. Kinematics and Physics of Celestial Bodies, 31, No. 2, 55–64. https://doi.org/10.3103/s0884591315020038
- Charbonneau P (2010). . Dynamo models of the solar cycle. Living Rev. Solar Phys., 7, No. 3, 1–91. https://doi.org/10.12942/lrsp-2010-3
- Solnechno-zemnye svyazi i kosmicheskaya pogoda (pod red. Petrukovicha A.A.) // Zelenyy L.M., Veselovsky I.S. (red.) Plazmennaya geliogeofizika. Tom II. – M.: Fizmatlit (2008). 560 p.
- Kremenets’kyy I.O., Cheremnykh O.K. (2009). Kosmichna pohoda: mekhanizmy i proyavy. Kyyiv: Naukova dumka. 144 p.
- Parnovskyy A.S., Ermolaev Yu.Y., Zhuk Y.T. (2010). Kosmycheskaya pohoda: ystoryya yssledovanyya y prohnozyrovany’e. Kosmichna nauka i tekhnolohiya, 16(1), 90–99.
- Kuznetsov V.D. (2012). Solnechno-zemnaya fizika i ee prilozheniya. UFN, 182(3), 327–326. https://doi.org/10.3367/ufnr.0182.201203h.0327
- Kuznetsov V.D. (2014). Kosmicheskaya pogoda i riski kosmicheskoy deyatel’nosti. Kosmicheskaya tekhnika i tekhnologii, 2014(3(6)), 327–326.
- Chizhevsky A.L. (1976). Zemnoe ekho solnechnykh bur’. M.: Mysl’. 368 p.
- Gibson E. (1977). Spokoynoe Solntse. M.: Mir. 408 p.
- Störmer C. (1918). La Theorie corpusculaire des aurores boreales. L'Astronomie, 32, 153–159; 200–205.
- Chapman S., Ferraro V.C.F. (1931). Terrest. Magn. and Atmosph. Elec., 77, 171. https://doi.org/10.1029/te036i003p00171
- Chapman S. (1954). The viscosity and thermal conductivity of a completely ionized gas. Astrophys. J., 120, 151. https://doi.org/10.1086/145890
- Biermann L. (1948). Über die Ursache der chromosphärischen Turbulenz und des UV-Exzesses der Sonnenstrahlung. Zs. f. Ap., 25, 161.
- Biermann L. (1952). Zs. f. Naturfororsch., 7a, 127.
- Parker E.N. (1958). Dynamics of the interplanetary gas and magnetic fields. Astrophys. J., 128, 664–676. https://doi.org/10.1086/146579
- Parker E.N. (1965). Dinamicheskie protsessy v mezhplanetnoy srede. M.: Mir. 364 p.
- Geliosfera (pod red Veselovskogo I.S., Ermolaeva Yu.I.) // Zelenyy L.M., Veselovsky I.S. (red.) Plazmennaya geliogeofizika. Tom I. – M.: Fizmatlit (2008). 560 p.
- Vsekhsvyatsky S.K., Nikol’sky G.M., Ponomarev E.A., Cherednichenko V.I. (1955). K voprosu o korpuskulyarnom izluchenii Solntsa. Astron. zhurnal., 32, 165–17.
- Ponomarev E.A. (1957). K teorii solnechnoy korony: Dissertatsiya na soiskanie uchenoy stepeni kandidata fiz.-mat. nauk. Kiev: Kievsky universitet. 233 p.
- Pudovkin M.I. (1996). Solnechnyy veter. Sorosovsky obrazovatel’nyy zhurnal, 1996(12), 87–94.
- Khundkhauzen A. Rasshirenie korony i solnechnyy veter. M.: Mir, 1976.
- Proelss G.W. Physics of the Earth's Space Environment. Berlin: Springer, 2004.
- Gazis P.R. (1996). Solar cycle variation in the heliosphere. Rev. Geophys., 34, No. 3, 379–402. https://doi.org/10.1029/96rg00892
- Sheeley N.R., Wang Y.-M., Hawley S.H., et al. (1997). Measurements of flow speeds in the corona between 2 and 30 Rsun. Astroph. J., 484, No. 1, 472–478. https://doi.org/10.1086/304338
- Wilcox J.M., Ness N.F. (1965). Extension of the photospheric magnetic field into interplanetary space. Astron. J., 70, 333. https://doi.org/10.1086/109608
- Forbush S.E. (1954). World-wide cosmic-ray variations, 1937–1952. J. Geophys. Res., 59, No. 4, 525–542. https://doi.org/10.1029/jz059i004p00525
Download PDF