The Solar Magnetic Field
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Arxiv:0906.0144V1 [Physics.Hist-Ph] 31 May 2009 Event
Solar physics at the Kodaikanal Observatory: A Historical Perspective S. S. Hasan, D.C.V. Mallik, S. P. Bagare & S. P. Rajaguru Indian Institute of Astrophysics, Bangalore, India 1 Background The Kodaikanal Observatory traces its origins to the East India Company which started an observatory in Madras \for promoting the knowledge of as- tronomy, geography and navigation in India". Observations began in 1787 at the initiative of William Petrie, an officer of the Company, with the use of two 3-in achromatic telescopes, two astronomical clocks with compound penduumns and a transit instrument. By the early 19th century the Madras Observatory had already established a reputation as a leading astronomical centre devoted to work on the fundamental positions of stars, and a principal source of stellar positions for most of the southern hemisphere stars. John Goldingham (1796 - 1805, 1812 - 1830), T. G. Taylor (1830 - 1848), W. S. Jacob (1849 - 1858) and Norman R. Pogson (1861 - 1891) were successive Government Astronomers who led the activities in Madras. Scientific high- lights of the work included a catalogue of 11,000 southern stars produced by the Madras Observatory in 1844 under Taylor's direction using the new 5-ft transit instrument. The observatory had recently acquired a transit circle by Troughton and Simms which was mounted and ready for use in 1862. Norman Pogson, a well known astronomer whose name is associated with the modern definition of the magnitude scale and who had considerable experience with transit instruments in England, put this instrument to good use. With the help of his Indian assistants, Pogson measured accurate positions of about 50,000 stars from 1861 until his death in 1891. -
Structure and Energy Transport of the Solar Convection Zone A
Structure and Energy Transport of the Solar Convection Zone A DISSERTATION SUBMITTED TO THE GRADUATE DIVISION OF THE UNIVERSITY OF HAWAI'I IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF DOCTOR OF PHILOSOPHY IN ASTRONOMY December 2004 By James D. Armstrong Dissertation Committee: Jeffery R. Kuhn, Chairperson Joshua E. Barnes Rolf-Peter Kudritzki Jing Li Haosheng Lin Michelle Teng © Copyright December 2004 by James Armstrong All Rights Reserved iii Acknowledgements The Ph.D. process is not a path that is taken alone. I greatly appreciate the support of my committee. In particular, Jeff Kuhn has been a friend as well as a mentor during this time. The author would also like to thank Frank Moss of the University of Missouri St. Louis. His advice has been quite helpful in making difficult decisions. Mark Rast, Haosheng Lin, and others at the HAO have assisted in obtaining data for this work. Jesper Schou provided the helioseismic rotation data. Jorgen Christiensen-Salsgaard provided the solar model. This work has been supported by NASA and the SOHOjMDI project (grant number NAG5-3077). Finally, the author would like to thank Makani for many interesting discussions. iv Abstract The solar irradiance cycle has been observed for over 30 years. This cycle has been shown to correlate with the solar magnetic cycle. Understanding the solar irradiance cycle can have broad impact on our society. The measured change in solar irradiance over the solar cycle, on order of0.1%is small, but a decrease of this size, ifmaintained over several solar cycles, would be sufficient to cause a global ice age on the earth. -
Solar Radiation
5 Solar Radiation In this chapter we discuss the aspects of solar radiation, which are important for solar en- ergy. After defining the most important radiometric properties in Section 5.2, we discuss blackbody radiation in Section 5.3 and the wave-particle duality in Section 5.4. Equipped with these instruments, we than investigate the different solar spectra in Section 5.5. How- ever, prior to these discussions we give a short introduction about the Sun. 5.1 The Sun The Sun is the central star of our solar system. It consists mainly of hydrogen and helium. Some basic facts are summarised in Table 5.1 and its structure is sketched in Fig. 5.1. The mass of the Sun is so large that it contributes 99.68% of the total mass of the solar system. In the center of the Sun the pressure-temperature conditions are such that nuclear fusion can Table 5.1: Some facts on the Sun Mean distance from the Earth 149 600 000 km (the astronomic unit, AU) Diameter 1392000km(109 × that of the Earth) Volume 1300000 × that of the Earth Mass 1.993 ×10 27 kg (332 000 times that of the Earth) Density(atitscenter) >10 5 kg m −3 (over 100 times that of water) Pressure (at its center) over 1 billion atmospheres Temperature (at its center) about 15 000 000 K Temperature (at the surface) 6 000 K Energy radiation 3.8 ×10 26 W TheEarthreceives 1.7 ×10 18 W 35 36 Solar Energy Internal structure: core Subsurface ows radiative zone convection zone Photosphere Sun spots Prominence Flare Coronal hole Chromosphere Corona Figure 5.1: The layer structure of the Sun (adapted from a figure obtained from NASA [ 28 ]). -
Magnetism, Dynamo Action and the Solar-Stellar Connection
Living Rev. Sol. Phys. (2017) 14:4 DOI 10.1007/s41116-017-0007-8 REVIEW ARTICLE Magnetism, dynamo action and the solar-stellar connection Allan Sacha Brun1 · Matthew K. Browning2 Received: 23 August 2016 / Accepted: 28 July 2017 © The Author(s) 2017. This article is an open access publication Abstract The Sun and other stars are magnetic: magnetism pervades their interiors and affects their evolution in a variety of ways. In the Sun, both the fields themselves and their influence on other phenomena can be uncovered in exquisite detail, but these observations sample only a moment in a single star’s life. By turning to observa- tions of other stars, and to theory and simulation, we may infer other aspects of the magnetism—e.g., its dependence on stellar age, mass, or rotation rate—that would be invisible from close study of the Sun alone. Here, we review observations and theory of magnetism in the Sun and other stars, with a partial focus on the “Solar-stellar connec- tion”: i.e., ways in which studies of other stars have influenced our understanding of the Sun and vice versa. We briefly review techniques by which magnetic fields can be measured (or their presence otherwise inferred) in stars, and then highlight some key observational findings uncovered by such measurements, focusing (in many cases) on those that offer particularly direct constraints on theories of how the fields are built and maintained. We turn then to a discussion of how the fields arise in different objects: first, we summarize some essential elements of convection and dynamo theory, includ- ing a very brief discussion of mean-field theory and related concepts. -
Rotational Cherecteristics of Solar Radio Emissions
Rotational charecteristics of solar radio emissions and IMF: A comparative study Mehul Mehta1, and Hari Om Vats2 1 VP & RPTP Science college, Vallabh Vidyanagar, 388 120, INDIA. meghdhanusha@yahoo,co.in 2 Physical Research Laboratory, Navrangpura, Ahmedabad, 380 009, INDIA. [email protected] Abstract In present work we have performed autocorrelation analysis of time series of disc integrated solar flux at 2800 MHz and daily observations of Interplanetary magnetic field (IMF) for the period of 1987 to 2010 to infer rotation period. The analysis presents a comparison between rotation periods obtained from radio emissions, a coronal feature and interplanetary magnetic field. The results show a correlation between two which indicates that IMF seems to emanate from regions of low latitudes while it is expected to originate from polar regions. 1.Introduction: The problem of solar rotation is being studied systematically since mid of 19th century. It was made clear that the Sun does not rotate like a solid body. Solar rotation is measured, mainly by two methods. One is observation of tracers like sunspots, faculae, filaments etc. and other is spectroscopic observations of Doppler shift of selected spectral lines. Each of these methods has its own limitations as pointed by Howard [1], in the review of observation and interpretation of solar rotation. In last two decades it has been shown by several groups that solar radio emissions can be used to estimate solar rotation [2,3 & 4] In this paper, we have used yet another method of inferring solar rotation using daily observations of solar radio emissions at 2800 MHz and interplanetary magnetic field (IMF). -
The Sun and the Solar Corona
SPACE PHYSICS ADVANCED STUDY OPTION HANDOUT The sun and the solar corona Introduction The Sun of our solar system is a typical star of intermediate size and luminosity. Its radius is about 696000 km, and it rotates with a period that increases with latitude from 25 days at the equator to 36 days at poles. For practical reasons, the period is often taken to be 27 days. Its mass is about 2 x 1030 kg, consisting mainly of hydrogen (90%) and helium (10%). The Sun emits radio waves, X-rays, and energetic particles in addition to visible light. The total energy output, solar constant, is about 3.8 x 1033 ergs/sec. For further details (and more accurate figures), see the table below. THE SOLAR INTERIOR VISIBLE SURFACE OF SUN: PHOTOSPHERE CORE: THERMONUCLEAR ENGINE RADIATIVE ZONE CONVECTIVE ZONE SCHEMATIC CONVECTION CELLS Figure 1: Schematic representation of the regions in the interior of the Sun. Physical characteristics Photospheric composition Property Value Element % mass % number Diameter 1,392,530 km Hydrogen 73.46 92.1 Radius 696,265 km Helium 24.85 7.8 Volume 1.41 x 1018 m3 Oxygen 0.77 Mass 1.9891 x 1030 kg Carbon 0.29 Solar radiation (entire Sun) 3.83 x 1023 kW Iron 0.16 Solar radiation per unit area 6.29 x 104 kW m-2 Neon 0.12 0.1 on the photosphere Solar radiation at the top of 1,368 W m-2 Nitrogen 0.09 the Earth's atmosphere Mean distance from Earth 149.60 x 106 km Silicon 0.07 Mean distance from Earth (in 214.86 Magnesium 0.05 units of solar radii) In the interior of the Sun, at the centre, nuclear reactions provide the Sun's energy. -
Solar Dynamo Wu Xuanyi Adviser: Prof
Solar dynamo Wu Xuanyi Adviser: Prof. Yuqing Lou, Prof. Xuening Bai 2019/05/24 OUTLINE • Introduction: sunspots and solar cycle • Solar dynamo model • α Ω dynamo • Interface dynamo (Babcock-Leighton mechanism) • Flux transport dynamo • Summary −4 Observation: sunspots 1G = 10 T earliest extant record of sunspots: Book of Changes dark spots on sun (Galileo) have lower temperature with respect to surrounding life time: days to weeks Regions of intense magnetic fields : 0.1~0.3T ( the normal magnetic field of sun is ~10G; for earth, 0.5G) Often in pairs: leading and trailing sunspots Hale’s polarity law: opposite polarity from north to south hemisphere;the polarity changes each solar cycle Observation: solar cycle • Sunspot activity changes spatially and periodically • Sunspot activity has a period of ~11 years with magnetic field reversed • Solar cycle ~ 22 years Sunspot activity caused by advection/diffusion? Induction equation: Advection Diffusion B ηB Reynolds number: diffusion time scale : = 2 τd L τd Lu Rm = = B uB τa η advection time scale : = τa L • Rm of sun>>1 => advection dominated; field line frozen in the plasma flow • But, the diffusion time scale of sun ~ 10 10 years ≫ solar cycle period • Need other mechanism to explain solar activities Solar dynamo theory A solar dynamo model should… • Sustain the magnetic field • Cyclic polarity of 11year period • Equator-ward migration of sunspots and pole-ward migration of diffuse surface field • Polar field strength • Observed antisymmetric parity • … Solar dynamo model • αΩ dynamo • Interface dynamo -
The Solar Core As Never Seen Before
The solar core as never seen before A. Eff-Darwich1;2, S.G. Korzennik3 1 Instituto de Astrof´ısicade Canarias (IAC), E-38200 La Laguna, Tenerife, Spain 2 Dept. de Edafolog´ıay Geolog´ıa,Universidad de La Laguna (ULL), E-38206 La Laguna, Tenerife, Spain 3 Harvard-Smithsonian Center for Astrophysics, 60 Garden St. Cambridge, MA,02138, USA E-mail: [email protected], [email protected] Abstract. One of the main drawbacks in the analysis of the dynamics of the solar core comes from the lack of consistent data sets that cover the low and intermediate degree range (` = 1; 200). It is usually necessary to merge data obtained from different instruments and/or fitting methodologies and hence one introduces undesired systematic errors. In contrast, we present the results of analyzing MDI rotational splittings derived by a single fitting methodology applied to 4608-, 2304-, etc..., down to 182-day long time series. The direct comparison of these data sets and the analysis of the numerical inversion results have allowed us to constrain the dynamics of the solar core and to establish the accuracy of these data as a function of the length of the time-series. 1. Introduction Ground-based helioseismic observations, e.g., GONG [5], and space-based ones, e.g., MDI [10] or GOLF [4], have allowed us to derive a good description of the dynamics of the solar interior [12], [2], [6]. Such helioseismic inferences have confirmed that the differential rotation observed at the surface persists throughout the convection zone. The outer radiative zone (0:3 < r=R < 0:7) appears to rotate approximately as a solid body at an almost constant rate (≈ 430 nHz), whereas the innermost core (0:19 < r=R < 0:3) rotates slightly faster than the rest of the radiative region. -
Solar and Heliospheric Magnetism in 5D
Heliophysics 2050 White Papers (2021) 4034.pdf Solar and Heliospheric Magnetism in 5D A. Pevtsov (NSO), T. Woods (CU/LASP), V. Martinez Pillet (NSO), D. Hassler (SwRI), T. Berger (CU/SWx TREC), S. Gosain (NSO), T. Hoeksema (Stanford U), A. Jones (CU/LASP), R. Kohnert (CU/LASP) Magnetic field in the solar atmosphere and heliosphere is a global, ever-changing, multi-scale system. Active regions that emerge, evolve, and decay in one “place” on the solar surface may cause small or big changes in other remote areas and in the extreme cases, over the whole solar corona. Small-scale instabilities could cause localized eruptions, or they may cascade to much larger scales, both across the “surface” and with height. Once the magnetized structures start erupting from the solar atmosphere, their magnetic systems may go through a complex reconnection process with overlaying large-scale fields including those rooted in solar polar areas. After it erupts, the magnetic system continues evolving as it travels towards Earth, Mars and beyond. In addition to spatial scales, magnetic fields may evolve on different time scales from rapid eruption processes to relatively slow evolutionary changes. To properly capture and study these changes in different spatial and temporal scales requires taking observations from multiple vantage points at sufficiently high time cadence, which we refer to as 5D concept (3D for three spatial directions, 1D time, and 1D magnetic field). The following six key inter-related science objectives are important to address before 2050 to advance the understanding of solar and heliospheric magnetism in 5D. 1. Understand the global interconnected magnetic system in the solar corona Active region emergence may cause magnetic field restructuring in remote locations (Zhang & Low 2001, 2002; Longcope et al. -
Strength and Phase of the Solar Dynamo During the Last 12 Cycles
1 Strength and phase of the solar dynamo during the last 12 cycles A. Ruzmaikin and J. Feynman Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California Short title: STRENGTH AND PHASE OF THE SOLAR DYNAMO DURING THE LAST 12 CYCLES 2 Abstract. We use the aa index of geomagnetic activity recorded for 130 years as a proxy for the strength and phase properties of the solar dynamo. To do this we spit the monthly aa into two parts; one proportional to the sunspot number and the other the residual. We argue that the first part it is a proxy for the solar toroidal magnetic field. The residual has the same periodicity and closely related amplitude but is shifted in phase. We relate this term to thesolar poloidal field generated from the toroidal field in the dynamo process. The changes in both components indicate a long-term trend in the strength and phase of the solar dynamo, perhaps related to 88 year Gleissberg cycle. Our results suggest a change in the distribution of the differential rotation and helicity distribution within the Sun’s convection zone over time scales of 50 years. 3 Introduction Solar activity is driven by a dynamo operating due to the Sun’sconvective motions including differential rotation and meridional circulation [Parker, 1979; Zeldovich et al., 19831. Although the solar magnetic field and the law governing the magnetic polarity of sunspots were discovered by G. Hale at the beginning of this century it was not until 1952 that the first observations of the poloidal field were made by H. -
A Forecast of Reduced Solar Activity and Its Implications for Nasa
A FORECAST OF REDUCED SOLAR ACTIVITY AND ITS IMPLICATIONS FOR NASA Kenneth Schatten and Heather Franz* a.i. solutions, Inc. ABSTRACT The “Solar Dynamo” method of solar activity forecasting is reviewed. Known generically as a “precursor” method, insofar as it uses observations which precede solar activity generation, this method now uses the Solar Dynamo Amplitude (SODA) Index to estimate future long-term solar activity. The peak amplitude of the next solar cycle (#24), is estimated at roughly 124 in terms of smoothed F10.7 Radio Flux and 74 in terms of the older, more traditional smoothed international or Zurich Sunspot number (Ri or Rz). These values are significantly smaller than the amplitudes of recent solar cycles. Levels of activity stay large for about four years near the peak in smoothed activity, which is estimated to occur near the 2012 timeflame. Confidence is added to the prediction of low activity by numerous examinations of the Sun’s weakened polar field. Direct measurements are obtained by the Mount Wilson Solar Observatory and the Wilcox Solar Observatory. Further support is obtained by examining the Sun’s polar faculae (bright features), the shape of coronal soft X-ray “holes,” and the shape of the “source surface” - a calculated coronal feature which maps the large scale structure of the Sun’s field. These features do not show the characteristics of well-formed polar coronal holes associated with typical solar minima. They show stunted polar field levels, which are thought to result in stunted levels of solar activity during solar cycle #24. The reduced levels of solar activity would have concomitant effects upon the space environment in which satellites orbit. -
The Solar System
The Solar System Our automated spacecraft have traveled to the Moon and to all the planets beyond our world The Sun appears to have been active for 4.6 billion years and has enough fuel for another 5 except Pluto; they have observed moons as large as small planets, flown by comets, and billion years or so. At the end of its life, the Sun will start to fuse helium into heavier elements sampled the solar environment. The knowledge gained from our journeys through the solar and begin to swell up, ultimately growing so large that it will swallow Earth. After a billion years system has redefined traditional Earth sciences like geology and meteorology and spawned an as a "red giant," it will suddenly collapse into a "white dwarf" -- the final end product of a star like entirely new discipline called comparative planetology. By studying the geology of planets, ours. It may take a trillion years to cool off completely. moons, asteroids, and comets, and comparing differences and similarities, we are learning more about the origin and history of these bodies and the solar system as a whole. We are also Mercury gaining insight into Earth's complex weather systems. By seeing how weather is shaped on other worlds and by investigating the Sun's activity and its influence through the solar system, Obtaining the first close-up views of Mercury was the primary objective of the Mariner 10 we can better understand climatic conditions and processes on Earth. spacecraft, launched Nov 3, 1973. After a journey of nearly 5 months, including a flyby of Venus, the spacecraft passed within 703 km (437 mi) of the solar system's innermost planet on Mar 29, The Sun 1974.