The Sun's Period of Rotation

Total Page:16

File Type:pdf, Size:1020Kb

The Sun's Period of Rotation The sun's period of rotation (adapted from the Universe at Your Fingertips) Procedure 1. Locate the major group of sunspots on the photographs in Figure 5. 2. Place the plastic overlay (Figure 4) on the photographs so that you can determine the latitude and longitude for the major sunspot group. Each vertical and horizontal line equals 10◦ latitude and longitude, respectively. 3. Estimate how far the sunspot group moves between day one and day two by subtracting the smaller longitude from the larger. Record this longitude change in the Table below. Estimate this number to the nearest whole degree. 4. Repeat the same process for the next days up to day four and record your results. 5. The Earth revolves around the Sun at a rate of 360 degrees in one year (365 days) or an average motion of about 1◦ per day. Since Earth revolves around the Sun in the same direction as the Sun rotates, our motion seems to chase after the sunspots. Thus, the apparent movement of sunspots is less than the real rotation by about 1◦ per day. Therefore, you must compensate for the orbital motion of Earth by adding 1◦ to your computed apparent daily motion. Add this result to column 4. 6. Let us assume that sunspots are features whose position on the Sun do not change very much over the course of a solar rotation. Use the following proportion to calculate the Sun's period of rotation (in days): corrected longitude change 360 degrees = 1 day X days 7. Find the average rotational period and record it in the Table below. Calculate to the nearest tenth of a day. Longitude of Sunspot Group Change in Longitude Corrected Longitude Change Period of Rotation (Ex: Day 2 - Day 1) (Solve for \X") Day 1 Day 2 Day 3 Day 4 Questions 1. Based on your calculations, what do you think is the period of the sun's rotation? How does this compare to the periods of Earth's rotation and Earth's orbit around the Sun? 1 2. Suppose you needed to get a much more accurate measurement of the sun's rotation. How might you achieve this? 3. Suppose you took photos of the sun separated by very short intervals (10 minutes) or very long intervals (100 days). Would you be able to determine the rotation period with either of these sets of measurements? Why or why not? 4. Compare the photo you took of the sun today with the photos in Figure 5. How are the two images similar, and how are they different? How do you explain these similarities and differences? 5. At some times in history, some cultures thought that all bodies in the sky were perfect - perfectly round and uniform, with no blemishes of any kind. Suppose you lived in one of these cultures and discovered sunspots on the sun. How would this change your view of the universe? What would you do with this information? Would you tell others, or would you be afraid to tell others? 6. Challenge question: Suppose the sun's period of rotation was exactly one year (365 days). How would the images in Figure 5 be different? 7. Challenge question: Suppose the Earth were closer to the sun and it took the Earth 180 days to orbit the sun. What correction would you need to apply to compute the correct change in longitude of the sunspots? 2.
Recommended publications
  • Effect of Solar Variability on the Earth's Climate Patterns
    Advances in Space Research 40 (2007) 1146–1151 www.elsevier.com/locate/asr Effect of solar variability on the Earth’s climate patterns Alexander Ruzmaikin Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA, USA Received 30 October 2006; received in revised form 8 January 2007; accepted 8 January 2007 Abstract We discuss effects of solar variability on the Earth’s large-scale climate patterns. These patterns are naturally excited as deviations (anomalies) from the mean state of the Earth’s atmosphere-ocean system. We consider in detail an example of such a pattern, the North Annular Mode (NAM), a climate anomaly with two states corresponding to higher pressure at high latitudes with a band of lower pres- sure at lower latitudes and the other way round. We discuss a mechanism by which solar variability can influence this pattern and for- mulate an updated general conjecture of how external influences on Earth’s dynamics can affect climate patterns. Ó 2007 COSPAR. Published by Elsevier Ltd. All rights reserved. Keywords: Solar irradiance; Climate and inter-annual variability; Solar variability impact; Climate dynamics 1. Introduction in solar irradiance. The solar cycle variations in total solar irradiance are small, 0.1%. However the magnitude of The center of attention of this paper is the response of irradiance variations strongly depends on the wavelength the Earth to solar variability on Space Climate time scales. and increases for the shorter wavelengths. Thus solar UV, In the context of Space Climate, the Earth can respond to which amounts to only a few percentage of the total irradi- solar variability on the 27-day solar rotation time scale, the ance, contributes 15% to the change in total irradiance 11-year solar cycle, the century scale Grand Minima, and (Lean et al., 2005).
    [Show full text]
  • Jupitor's Great Red Spot
    GREAT RED SPOT appears somewhat orange in this remarkably ly ranged from '.'full gray" and "pinkish" to "brick red" and "car· detailed photograph made at the Lunar and Planetary Laboratory mine." The photograph was made on December 23, 1966, by Alika of the University of Arizona. During the century or so that Jupiter's Herring and John Fountain, who used a 61·inch reflecting tele· great red spot bas been closely observed its color has reported. scope. The exposure was one second on High Speed Ektachrome. © 1968 SCIENTIFIC AMERICAN, INC JUPITER'S GREAT RED SPOT There is evidence to suggest that this peculiar Inarking is the top of a "Taylor cohunn": a stagnant region above a bll111p 01' depression at the botton1 of a circulating fluid by Haymond Hide he surface markings of the plan­ To explain the fluctuations in the red tals suspended in an atmosphere that is Tets have always had a special fas­ spot's period of rotation one must assume mainly hydrogen admixed with water cination, and no single marking that there are forces acting on the solid and perhaps methane and helium. Other has been more fascinating and puzzling planet capable of causing an equivalent lines of evidence, particularly the fact than the great red spot of Jupiter. Un­ change in its rotation period. In other that Jupiter's density is only 1.3 times like the elusive "canals" of Mars, the red words, the fluctuations in the rotation the density of water, suggest that the spot unmistakably exists. Although it has period of the red spot are to be regarded main constituents of the planet are hy­ been known to fade and change color, it as a true reflection of the rotation period drogen and helium.
    [Show full text]
  • SPITZER SPACE TELESCOPE MID-IR LIGHT CURVES of NEPTUNE John Stauffer1, Mark S
    The Astronomical Journal, 152:142 (8pp), 2016 November doi:10.3847/0004-6256/152/5/142 © 2016. The American Astronomical Society. All rights reserved. SPITZER SPACE TELESCOPE MID-IR LIGHT CURVES OF NEPTUNE John Stauffer1, Mark S. Marley2, John E. Gizis3, Luisa Rebull1,4, Sean J. Carey1, Jessica Krick1, James G. Ingalls1, Patrick Lowrance1, William Glaccum1, J. Davy Kirkpatrick5, Amy A. Simon6, and Michael H. Wong7 1 Spitzer Science Center (SSC), California Institute of Technology, Pasadena, CA 91125, USA 2 NASA Ames Research Center, Space Sciences and Astrobiology Division, MS245-3, Moffett Field, CA 94035, USA 3 Department of Physics and Astronomy, University of Delaware, Newark, DE 19716, USA 4 Infrared Science Archive (IRSA), 1200 E. California Boulevard, MS 314-6, California Institute of Technology, Pasadena, CA 91125, USA 5 Infrared Processing and Analysis Center, MS 100-22, California Institute of Technology, Pasadena, CA 91125, USA 6 NASA Goddard Space Flight Center, Solar System Exploration Division (690.0), 8800 Greenbelt Road, Greenbelt, MD 20771, USA 7 University of California, Department of Astronomy, Berkeley CA 94720-3411, USA Received 2016 July 13; revised 2016 August 12; accepted 2016 August 15; published 2016 October 27 ABSTRACT We have used the Spitzer Space Telescope in 2016 February to obtain high cadence, high signal-to-noise, 17 hr duration light curves of Neptune at 3.6 and 4.5 μm. The light curve duration was chosen to correspond to the rotation period of Neptune. Both light curves are slowly varying with time, with full amplitudes of 1.1 mag at 3.6 μm and 0.6 mag at 4.5 μm.
    [Show full text]
  • Mercury Friday, February 23
    ASTRONOMY 161 Introduction to Solar System Astronomy Class 18 Mercury Friday, February 23 Mercury: Basic characteristics Mass = 3.302×1023 kg (0.055 Earth) Radius = 2,440 km (0.383 Earth) Density = 5,427 kg/m³ Sidereal rotation period = 58.6462 d Albedo = 0.11 (Earth = 0.39) Average distance from Sun = 0.387 A.U. Mercury: Key Concepts (1) Mercury has a 3-to-2 spin-orbit coupling (not synchronous rotation). (2) Mercury has no permanent atmosphere because it is too hot. (3) Like the Moon, Mercury has cratered highlands and smooth plains. (4) Mercury has an extremely large iron-rich core. (1) Mercury has a 3-to-2 spin-orbit coupling (not synchronous rotation). Mercury is hard to observe from the Earth (because it is so close to the Sun). Its rotation speed can be found from Doppler shift of radar signals. Mercury’s unusual orbit Orbital period = 87.969 days Rotation period = 58.646 days = (2/3) x 87.969 days Mercury is NOT in synchronous rotation (1 rotation per orbit). Instead, it has 3-to-2 spin-orbit coupling (3 rotations for 2 orbits). Synchronous rotation (WRONG!) 3-to-2 spin-orbit coupling (RIGHT!) Time between one noon and the next is 176 days. Sun is above the horizon for 88 days at the time. Daytime temperatures reach as high as: 700 Kelvin (800 degrees F). Nighttime temperatures drops as low as: 100 Kelvin (-270 degrees F). (2) Mercury has no permanent atmosphere because it is too hot (and has low escape speed). Temperature is a measure of the 3kT v = random speed of m atoms (or v typical speed of atom molecules).
    [Show full text]
  • How to Calculate Planetary-Rotation Periods
    Explaining Planetary-Rotation Periods Using an Inductive Method Gizachew Tiruneh, Ph. D., Department of Political Science, University of Central Arkansas (First submitted on June 19th, 2009; last updated on June 15th, 2011) This paper uses an inductive method to investigate the factors responsible for variations in planetary-rotation periods. I began by showing the presence of a correlation between the masses of planets and their rotation periods. Then I tested the impact of planetary radius, acceleration, velocity, and torque on rotation periods. I found that velocity, acceleration, and radius are the most important factors in explaining rotation periods. The effect of mass may be rather on influencing the size of the radii of planets. That is, the larger the mass of a planet, the larger its radius. Moreover, mass does also influence the strength of the rotational force, torque, which may have played a major role in setting the initial constant speeds of planetary rotation. Key words: Solar system; Planet formation; Planet rotation Many astronomers believe that planetary rotation is influenced by angular momentum and related phenomena, which may have occurred during the formation of the solar system (Alfven, 1976; Safronov, 1995; Artemev and Radzievskii, 1995; Seeds, 2001; Balbus, 2003). There is, however, not much identifiable recent research on planetary-rotation periods. Hughes’ (2003) review of the literature reveals that much research is needed to understand the phenomenon of planetary spin. Some of the assumptions that scholars have made in the past, according to Hughes (2003), include that planetary spin is a function of the gaseous or terrestrial nature of planets, that there is a power law relationship between planetary spin angular momentum and planetary mass, that there is a relationship between planets’ escape velocities and their spin rates, and that mass-independent spin periods can be obtained if one posits that a planetary formation process is governed by the balance between gravitational and centrifugal forces at the planetary equator.
    [Show full text]
  • Determining the Rotation Period of the Sun
    SOLAR PHYSICS AND TERRESTRIAL EFFECTS 2+ Activity 8 4= Activity 8 Determining the Rotation Period of the Sun Relevant Reading Chapter 2, section 3 Purpose Determine the rotation period of the Sun. Although numerous methods for accurate measurement are used in solar research, the method described here, using photographs taken over several days, will allow determination to within an Earth-day. Materials Photo set that shows at least one solar feature that can be followed over a several-day period. For real challenge, take the photos yourself, or make a simple projection sketch of sunspots over several days. 1 sheet of clear plastic used for overhead transparencies or viewgraphs, or something similar such as a clear plastic report folder a mm ruler, compass and protractor a fine-tipped marking pen suitable for plastic graph paper with 1-mm squares Procedures 1. Measure, to the nearest millimeter, the diameter of the Sun on the photo taken near the middle of the data period. 2. Use a compass and draw a circle with the same diameter on the transpar- ent sheet. 3. With the circle aligned over the photo on the date used for the diameter, trace the axis orientation marks onto the transparency. 4. Pick a solar feature that traverses the solar disk for as many days as pos- sible. Align the circle on the transparency over each successive photo and carefully mark the position of the chosen solar feature along with its date. 5. Carefully draw the best fitting straight line through the marked positions and measure its length across the circle as accurately as possible.
    [Show full text]
  • Venus Lithograph
    National Aeronautics and and Space Space Administration Administration 0 300,000,000 900,000,000 1,500,000,000 2,100,000,000 2,700,000,000 3,300,000,000 3,900,000,000 4,500,000,000 5,100,000,000 5,700,000,000 kilometers Venus www.nasa.gov Venus and Earth are similar in size, mass, density, composi- and at the surface are estimated to be just a few kilometers per SIGNIFICANT DATES tion, and gravity. There, however, the similarities end. Venus hour. How this atmospheric “super-rotation” forms and is main- 650 CE — Mayan astronomers make detailed observations of is covered by a thick, rapidly spinning atmosphere, creating a tained continues to be a topic of scientific investigation. Venus, leading to a highly accurate calendar. scorched world with temperatures hot enough to melt lead and Atmospheric lightning bursts, long suspected by scientists, were 1761–1769 — Two European expeditions to watch Venus cross surface pressure 90 times that of Earth (similar to the bottom confirmed in 2007 by the European Venus Express orbiter. On in front of the Sun lead to the first good estimate of the Sun’s of a swimming pool 1-1/2 miles deep). Because of its proximity Earth, Jupiter, and Saturn, lightning is associated with water distance from Earth. to Earth and the way its clouds reflect sunlight, Venus appears clouds, but on Venus, it is associated with sulfuric acid clouds. 1962 — NASA’s Mariner 2 reaches Venus and reveals the plan- to be the brightest planet in the sky. We cannot normally see et’s extreme surface temperatures.
    [Show full text]
  • The Evolution of the Earth-Moon System Based on the Dark Fluid Model
    The evolution of the Earth-Moon system based on the dark matter field fluid model Hongjun Pan Department of Chemistry University of North Texas, Denton, Texas 76203, U. S. A. Abstract The evolution of Earth-Moon system is described by the dark matter field fluid model with a non-Newtonian approach proposed in the Meeting of Division of Particle and Field 2004, American Physical Society. The current behavior of the Earth-Moon system agrees with this model very well and the general pattern of the evolution of the Moon-Earth system described by this model agrees with geological and fossil evidence. The closest distance of the Moon to Earth was about 259000 km at 4.5 billion years ago, which is far beyond the Roche’s limit. The result suggests that the tidal friction may not be the primary cause for the evolution of the Earth-Moon system. The average dark matter field fluid constant derived from Earth-Moon system data is 4.39 × 10-22 s-1m-1. This model predicts that the Mars’s rotation is also slowing with the angular acceleration rate about -4.38 × 10-22 rad s-2. Key Words. dark matter, fluid, evolution, Earth, Moon, Mars 1 1. Introduction The popularly accepted theory for the formation of the Earth-Moon system is that the Moon was formed from debris of a strong impact by a giant planetesimal with the Earth at the close of the planet-forming period (Hartmann and Davis 1975). Since the formation of the Earth-Moon system, it has been evolving at all time scale.
    [Show full text]
  • Constraining Ceres' Interior from Its Rotational Motion
    A&A 535, A43 (2011) Astronomy DOI: 10.1051/0004-6361/201116563 & c ESO 2011 Astrophysics Constraining Ceres’ interior from its rotational motion N. Rambaux1,2, J. Castillo-Rogez3, V. Dehant4, and P. Kuchynka2,3 1 Université Pierre et Marie Curie, UPMC–Paris 06, France e-mail: [nicolas.rambaux;kuchynka]@imcce.fr 2 IMCCE, Observatoire de Paris, CNRS UMR 8028, 77 avenue Denfert-Rochereau, 75014 Paris, France 3 Jet Propulsion Laboratory, Caltech, Pasadena, USA e-mail: [email protected] 4 Royal Observatory of Belgium, 3 avenue Circulaire, 1180 Brussels, Belgium Received 24 January 2011 / Accepted 14 July 2011 ABSTRACT Context. Ceres is the most massive body of the asteroid belt and contains about 25 wt.% (weight percent) of water. Understanding its thermal evolution and assessing its current state are major goals of the Dawn mission. Constraints on its internal structure can be inferred from various types of observations. In particular, detailed knowledge of the rotational motion can help constrain the mass distribution inside the body, which in turn can lead to information about its geophysical history. Aims. We investigate the signature of internal processes on Ceres rotational motion and discuss future measurements that can possibly be performed by the spacecraft Dawn and will help to constrain Ceres’ internal structure. Methods. We compute the polar motion, precession-nutation, and length-of-day variations. We estimate the amplitudes of the rigid and non-rigid responses for these various motions for models of Ceres’ interior constrained by shape data and surface properties. Results. As a general result, the amplitudes of oscillations in the rotation appear to be small, and their determination from spaceborne techniques will be challenging.
    [Show full text]
  • Lecture 21: Venus
    Lecture 21: Venus 1 Venus Terrestrial Planets Animation Venus •The orbit of Venus is almost circular, with eccentricity e = 0.0068 •The average Sun-Venus distance is 0.72 AU (108,491,000 km) •Like Mercury, Venus always appears close to the Sun in the sky Venus 0.72 AU 47o 1 AU Sun Earth 2 Venus •Venus is visible for no more than about three hours •The Earth rotates 360o in 24 hours, or o o 360 = 15 24 hr hr •Since the maximum elongation of Venus is 47o, the maximum time for the Sun to rise after Venus is 47o ∆ t = ≈ 3 hours 15o / hr Venus •The albedo of an object is the fraction of the incident light that is reflected Albedo = 0.1 for Mercury Albedo = 0.1 for Moon Albedo = 0.4 for Earth Albedo = 0.7 for Venus •Venus is the third brightest object in the sky (Sun, Moon, Venus) •It is very bright because it is Close to the Sun Fairly large (about Earth size) Highly reflective (large albedo) Venus •Where in its orbit does Venus appears brightest as viewed from Earth? •There are two competing effects: Venus appears larger when closer The phase of Venus changes along its orbit •Maximum brightness occurs at elongation angle 39o 3 Venus •Since Venus is closer to the Sun than the Earth is, it’s apparent motion can be retrograde •Transits occur when Venus passes in front of the solar disk as viewed from Earth •This happens about once every 100 years (next one is in 2004) Venus (2 hour increments) Orbit of Venus •The semi-major axis of the orbit of Venus is a = 0.72 AU Venus Sun a •Kepler’s third law relates the semi-major axis to the orbital period
    [Show full text]
  • Origin of the Earth and Moon Conference 4075.Pdf
    Origin of the Earth and Moon Conference 4075.pdf INFERENCES ABOUT THE EARLY MOON FROM GRAVITY AND TOPOGRAPHY. D. E. Smith1 and M. T. Zu- ber2,1, 1Laboratory for Terrestrial Physics, Code 920, NASA/Goddard Space Flight Center, Greenbelt MD 20771, USA ([email protected]), 2Department of Earth, Atmospheric and Planetary Sciences, 54-518, Massachusetts Institute of Technology, Cambridge MA 02139, USA ([email protected],gov). Recent spacecraft missions to the Moon [1,2] have sig- If the Moon behaved like a perfect fluid then the present nificantly improved our knowledge of the lunar gravity and nearside tidal bulge would be about 10 m. For the tide to topography fields and have raised some new and old ques- approach 770 m, the Moon must have been over 4 times tions about the early lunar history [3]. It has frequently closer to Earth (~15 REarth) than it is at present and would been assumed that the shape of the Moon today reflects an have a rotation period of only about 3.5 days. In this orbit earlier equilibrium state and that the Moon has retained the effective permanent tide at the lunar poles would be some internal strength. Recent analysis indicating a superi- about 650 m, which would decrease the flattening and in- sostatic state of some lunar basins [4] lends support to this crease the distance of the Moon required to obtain the req- hypothesis. uisite rotation. Combining the tidal effect estimated from On its simplest level the present shape of the Moon is the equatorial ellipticity and the rotation leads to a lunar slightly flattened by 2.2 ± 0.2 km [5] while its gravity field, period of nearly 3 days at a distance of slightly more than 13 represented by an equipotential surface, is flattened only REarth (Fig.
    [Show full text]
  • Solar Differential Rotation in the Period 1964–2016 Determined by the Kanzelhöhe Data Set
    A&A 606, A72 (2017) Astronomy DOI: 10.1051/0004-6361/201731047 & c ESO 2017 Astrophysics Solar differential rotation in the period 1964–2016 determined by the Kanzelhöhe data set I. Poljanciˇ c´ Beljan1, R. Jurdana-Šepic´1, R. Brajša2, D. Sudar2, D. Ruždjak2, D. Hržina3, W. Pötzi4, A. Hanslmeier5, A. Veronig4; 5, I. Skokic´6, and H. Wöhl7 1 Physics Department, University of Rijeka, Radmile Matejciˇ c´ 2, 51000 Rijeka, Croatia e-mail: [email protected] 2 Hvar Observatory, Faculty of Geodesy, University of Zagreb, Kaciˇ ceva´ 26, 10000 Zagreb, Croatia 3 Zagreb Astronomical Observatory, Opatickaˇ 22, 10000 Zagreb, Croatia 4 Kanzelhöhe Observatory for Solar and Environmental Research, University of Graz, Kanzelhöhe 19, 9521 Treffen am Ossiacher See, Austria 5 Institute for Geophysics, Astrophysics and Meteorology, Institute of Physics, University of Graz, Universitätsplatz 5, 8010 Graz, Austria 6 Astronomical Institute of the Czech Academy of Sciences, Fricovaˇ 298, 25165 Ondrejov,ˇ Czech Republic 7 Kiepenheuer-Institut für Sonnenphysik, Schöneckstr. 6, 79104 Freiburg, Germany Received 26 April 2017 / Accepted 5 July 2017 ABSTRACT Context. Kanzelhöhe Observatory for Solar and Environmental Research (KSO) provides daily multispectral synoptic observations of the Sun using several telescopes. In this work we made use of sunspot drawings and full disk white light CCD images. Aims. The main aim of this work is to determine the solar differential rotation by tracing sunspot groups during the period 1964–2016, using the KSO sunspot drawings and white light images. We also compare the differential rotation parameters derived in this paper from the KSO with those collected fromf other data sets and present an investigation of the north – south rotational asymmetry.
    [Show full text]