Uppsala universitet Institutionen för astronomi och rymdfysik Anders Eriksson

Similar documents
Tentamen för kursen Rymdfysik (1FA255)

Uppsala universitet Institutionen för astronomi och rymdfysik Anders Eriksson och Jan-Erik Wahlund

Single Particle Motion in a Magnetized Plasma

Chapter 8 Geospace 1

Space Physics. An Introduction to Plasmas and Particles in the Heliosphere and Magnetospheres. May-Britt Kallenrode. Springer

cos 6 λ m sin 2 λ m Mirror Point latitude Equatorial Pitch Angle Figure 5.1: Mirror point latitude as function of equatorial pitch angle.

Single particle motion and trapped particles

Earth s Magnetosphere

The Magnetic Sun. CESAR s Booklet

The Structure of the Magnetosphere

David versus Goliath 1

! The Sun as a star! Structure of the Sun! The Solar Cycle! Solar Activity! Solar Wind! Observing the Sun. The Sun & Solar Activity

Introduction to Plasma Physics

ESS 7 Lectures 21 and 22 November 21 and 24, The Planets

PROBLEM 1 (15 points) In a Cartesian coordinate system, assume the magnetic flux density

Magnetospheric Currents at Quiet Times

Remote sensing of magnetospheric processes: Lesson 1: Configura7on of the magnetosphere

The Physics of Field-Aligned Currents

This project has received funding from the European Union s Horizon 2020 research and innovation programme under the Marie-Sklodowska-Curie grant

Introduction to the Sun and the Sun-Earth System

How is Earth s Radiation Belt Variability Controlled by Solar Wind Changes

Global Monitoring of the Terrestrial Ring Current

Magnetic Reconnection

ESS 200C. Lectures 6 and 7 The Solar Wind

Single particle motion

CHARGED PARTICLE MOTION IN CONSTANT AND UNIFORM ELECTROMAGNETIC FIELDS

SW103: Lecture 2. Magnetohydrodynamics and MHD models

Space weather. Introduction to lectures by Dr John S. Reid. Image courtesy:

Plasma collisions and conductivity

Global MHD Eigenmodes of the Outer Magnetosphere

Physical Science Context Lecture 2 The Earth and Sun's Magnetic Fields

NASA Future Magnetospheric Missions. J. Slavin & T. Moore Laboratory for Solar & Space Physics NASA GSFC

The Sun sends the Earth:

Zach Meeks. Office: Ford ES&T Phone: (918) Please let me know if you have any questions!

Space Physics: Recent Advances and Near-term Challenge. Chi Wang. National Space Science Center, CAS

ESS 7. October 18, 22, and 25. The Magnetosphere

ESS 200C Aurorae. Lecture 15

The Solar wind - magnetosphere - ionosphere interaction

Planetary magnetospheres

BravoSat: Optimizing the Delta-V Capability of a CubeSat Mission. with Novel Plasma Propulsion Technology ISSC 2013

Introduction to Space Weather

Lecture 3: The Earth, Magnetosphere and Ionosphere.

1.2 Which parameters are used to characterize a plasma? Briefly discuss their physical meaning.

Planetary Magnetospheres

Plasma Interactions with Electromagnetic Fields

Numerical Studies of Spacecraft-Plasma Interaction: Simulations of Wake Effects on the Cluster Electric Field Instrument EFW

The Sun Our Star. Properties Interior Atmosphere Photosphere Chromosphere Corona Magnetism Sunspots Solar Cycles Active Sun

Geomagnetic storms. Measurement and forecasting

In-Situ vs. Remote Sensing

Spacecraft Environment! Launch Phases and Loading Issues-1

DIN EN : (E)

CESAR BOOKLET General Understanding of the Sun: Magnetic field, Structure and Sunspot cycle

Radiation belt particle dynamics

Planetary Magnetospheres: Homework Problems

Solar-Wind/Magnetosphere Coupling

Earth s Magnetic Field

Venus and Mars Observing Induced Magnetospheres

An introduction to the plasma state in nature and in space

Questions from April 2003 Physics Final Exam

Living in a Star. Sarah Gibson (NCAR/HAO)

Time Series of Images of the Auroral Substorm

High energy particles from the Sun. Arto Sandroos Sun-Earth connections

Space Weather. ~ Affects of solar activities onto Earth. Cause-Effect Time Intervals range from immediate (precisely, 8 minutes) to several days.

Single Particle Motion

Cosmic Rays - R. A. Mewaldt - California Institute of Technology

Response of the Earth s magnetosphere and ionosphere to the small-scale magnetic flux rope in solar wind by the MHD simulation

p = nkt p ~! " !" /!t + # "u = 0 Assumptions for MHD Fluid picture !du/dt = nq(e + uxb) " #p + other Newton s 2nd law Maxwell s equations

Planned talk schedule. Substorm models. Reading: Chapter 9 - SW-Magnetospheric Coupling from Russell book (posted)

Your web browser (Safari 7) is out of date. For more security, comfort and the best experience on this site: Update your browser Ignore

DYNAMICS OF THE EARTH S MAGNETOSPHERE

Tilts and Obliquities!

Sun Earth Connection Missions

Atmospheric Structure

Force on a Moving Charge in a Magnetic Field: Examples and Applications

Atmospheric escape. Volatile species on the terrestrial planets

Chapter 9 The Sun. Nuclear fusion: Combining of light nuclei into heavier ones Example: In the Sun is conversion of H into He

Ion Dynamics in Magnetic Reconnection Region

Andrew Keen, Inari, Finland 18 Feb º C spaceweather.com

Space Weather and Satellite System Interaction

Figure 1.1: Ionization and Recombination

Collisions and transport phenomena

YOUR NAME Sample Final Physics 1404 (Dr. Huang)), Correct answers are underlined.

Lecture 14: Solar Cycle. Observations of the Solar Cycle. Babcock-Leighton Model. Outline

Solar Winds. N.G. Schultheiss translated and adapted by K. Schadenberg. This module follows upon The Sun and can be continued by Cosmic Radiation.

Stars, Galaxies & the Universe Announcements. Stars, Galaxies & the Universe Lecture Outline. Exterior Layers of the Sun: HW#5 due Friday by 5 pm!

Reduced MHD. Nick Murphy. Harvard-Smithsonian Center for Astrophysics. Astronomy 253: Plasma Astrophysics. February 19, 2014

1. (a) Describe the difference between over-expanded, under-expanded and ideallyexpanded

Magnetism and You. Fields

The Physics of Space Plasmas

SATELLITE ABSORPTION OF ENERGETIC PARTICLES

MAE 5595: Space Environments and Spacecraft Interactions. Lesson 4: Introduction

Substorms at Mercury: Old Questions and New Insights. Daniel N. Baker Laboratory for Atmospheric and Space Physics (LASP)

The Sun. How are these quantities measured? Properties of the Sun. Chapter 14

Magnetospheric Physics - Homework, 02/21/ Local expansion of B: Consider the matrix B = (1)

Physics 12 January 2001 Provincial Examination

Introductory Lecture II: An Overview of Space Storms

The Solar Resource: The Active Sun as a Source of Energy. Carol Paty School of Earth and Atmospheric Sciences January 14, 2010

Introduction to the Sun-Earth system Steve Milan

Space Plasma Physics at the University of Minnesota

Satellite Orbital Maneuvers and Transfers. Dr Ugur GUVEN

Transcription:

Tentamen för Rymdfysik I 2006-08-15 Uppsala universitet Institutionen för astronomi och rymdfysik Anders Eriksson Please write your name on all papers, and on the first page your address, e-mail and phone number as well. Answers may of course be given in Swedish or English, according to your own preference. Time: 09:00-14:00 Allowed tools: Mathematics Handbook, Physics Handbook, enclosed formula sheet, calculator. A bilingual dictionary, for example English-Swedish or English-French, may also be used. 1. Here follows a set of multiple choice questions, where you must find out which statements are correct. For each question 1-1, 1-2 etc), there is only one correct combination of answers, say A and B or none. To score on a question, you need to have exactly the right combination. You are welcome to add comments to your answers. Any number of alternatives can be correct 0 3). 1 p/question, 10 p in total) 1:1. Reconnection and substorms: A. Reconnection is the common mechanism driving explosive magnetic events like solar flares and geomagnetic substorms. B. During reconnection, magnetic energy is converted to particle energy in the plasma. C. The energy released in a geomagnetic substorm has been stored in the geomagnetic tail. 1:2. Solar activity: A. The activity of the sun varies in a 22-year cycle. If the last solar maximum was around year 2000, the next solar maximum will be around 2022. B. The intensity of visible light from the sun drops by around 50% from solar maximum to solar minimum. C. The sunspot number anticorrelates with the solar activity: more sunspots means the sun is colder and less active. 1:3. Rockets and propulsion: A. For rocket launches from Earth, the only important parameter is the total impulse of the rocket, F,, not the force F itself. B. Rockets are often launched westwards to take advantage of the rotation of the Earth. C. The fraction of mass that is fuel can be as high as 90% for a rocket ready for launch. 1:4. Magnetosphere: A. The magnetosphere disappears at nighttime, because the ionization by solar radiation then stops. B. Electrical currents flow on the magnetopause, which is the outer boundary of the magnetosphere. C. The radiation belts van Allen bets) contain trapped energetic protons and electrons. 1:5. Solar wind: A. The solar wind is supersonic i.e. it blows faster than the sound speed in itself). 1

B. The solar wind blows out through the solar system in a spiral pattern as seen in an inertial frame). C. The typical solar wind speed at Earth orbit is in the range 200 600 km/s. 1:6. Motion of charged particles: A. The orbital magnetic moment of an electron moving in a magnetic field is conserved if the field varies only a little during an electron gyroperiod or inside an electron gyroradius. B. In a hydrogen plasma in thermodynamic equilibrium, electrons move much faster than protons. C. An electric field perpendicular to a magnetic field does not give rise to any electric currents in a collissionless plasma. 1:7. Plasmas: A. A plasma is a gas of charged particles. B. Plasmas are usually dominated by ions. The electrons are almost always only a small fraction of the total number of particles. C. The electric field on large scales in space and time is usually related to the flow velocity and the magnetic field by the relation E v + B = 0. 1:8. Ionosphere: A. The electron density in the dayside ionosphere is determined by the solar UV intensity and the Earth s atmospheric density. B. Due to collissions between particles, the conductivity in the direction parallel to the magnetic field is lower in the ionosphere than in the magnetosphere. C. Field-aligned currents can flow along the magnetic field from the magnetic tail into the ionosphere, flow perpendicular to B in the ionosphere, and then flow up along the magnetic field lines from a different part of the ionosphere. 1:9. Aurora: A. The aurora is mainly caused by electrons from the sun, hitting the Earth s atmosphere at the poles. B. The aurora is mainly caused by electrons accelerated inside the Earth s magnetosphere in regions where field-aligned currents flow. C. The main reason why auroras are easier to see in Kiruna than in Berlin in winter is that the sky in Kiruna is darker, so that the aurora can easily be detected. 1:10. Which statements about temperatures are correct? A. The equilibrium temperature of an interplanetary spacecraft, travelling between e.g. Earth and Mars, is determined by the temperature of the solar wind plasma around 10 ev). B. The equilibrium temperature of an interplanetary spacecraft, travelling between e.g. Earth and Mars, is determined by the balance between absorbtion of solar radiation and emission of thermal radiation. C. The equilibrium temperature of an interplanetary spacecraft, travelling between e.g. Earth and Mars, is determined by the cosmic microwave background radiation temperature around 2.7 K). 2

Figure 1: The ground track of Freja between 9:00 and 11:00 UT on June 13, 1995 2. Consider a spacecraft formed as a rectangular box of 2 x 2 x 4 m, with uniform surface properties and good thermal conductivity. At a distance of 1 AU from the sun, the equilibrium temperature of the spacecraft is 30 C when one of the 2 x 2 m surfaces points to the sun and all internal heating sources are turned off. When an electrical equipment producing 15 W was turned on, the temperature rose to 32 C. Calculate the absorbtion and emission coefficients. 3 p) 3. The Swedish-German Freja satellite was launched in October 1992 into a near-circular, eastward orbit around the Earth, with inclination 63 and orbital period 1 h 50 min. For the calculations here, we assume the geomagnetic field to be a dipole field of strength 30 µt on the ground at the equator, with dipole axis parallel to the Earth s spin axis. a) The ground track of Freja for two hours is shown in Figure 1. If the orbital period is 1 h 50 min as said above, why isn t the orbit closed in this plot? 1 p) b) Calculate Freja s speed and altitude height above the Earth), and also give the inclination of the Freja orbit. 2 p) c) What is the strongest magnetic field in µt) you expect the magnetometer onboard Freja should measure? In addition, mark on the map in Figure 1 where in the orbit this maximal value is seen. 2 p) d) Assume the plasma to be co-rotating with the Earth, and the electric field in the plasma to be zero. What is the value and direction of the electric field measured by the Freja electric field instrument at the points) of maximum magnetic field strength? 2 p) 4. Consider an oxygen ion O + ) with a kinetic energy of 1 MeV and no velocity along the magnetic field, moving in the equatorial plane at a distance of 4 R E from the center of the Earth. Calculate the drift period for this particle, i.e. the time it takes to complete on full orbit around the Earth. The geomagnetic field may be taken to be a dipole field with strength 30 µt on the ground at the equator. 3 p) 5. Consider the following model of the magnetic field in the central part of the geomagnetic tail: B 0ˆx, z < a Br) = B 0 ˆx 3 a2 z z 3 2 a, a z a 3 B 0ˆx, z > a 3

z x Figure 2: Idealized geometry of the relevant part of the geomagnetic tail around the origin). where B 0 = 1 nt, a = 2000 km and the coordinates are defined as in Figure 2. a) Calculate the current density jr) and the magnetic force density jr) Br) magnitudes and directions as functions of position). Also calculate their numerical values at z = 0. 3 p) b) How can such a current be sustained? Sketch possible orbits of ions and electrons in the y-z-plane that is, not the plane of Figure 2, but a plane cutting it at right angles at x = 0, and tell why the trajectories look as you have drawn them, with reference to some relevant equation. 2 p) c) Now consider what happens if an instability appears in the region a < x < a, 10 a < y < 10 a, a < z < a so that the resistivity in this region includes drastically. When the currents cannot flow through this region as before, where will they close now? Is this example relevant for any phenomenon in Earth s magnetosphere? 2 p) Lycka till! 4

Space Physics Formulas: Complement to Physics Handbook Charge density in plasma with charge particle species s: ρ = s q s n s Current density: j = s q s n s v s Dipole magnetic field: Dipole field lines: Magnetic field energy density and pressure: Equation of motion of neutral gas: ) 3 R0 Br, θ) = B 0 2ˆr cos θ + ˆθ sin θ) r ρ m dv Equation of motion of gas of charged particles: MHD equation of motion: Equation of continuity: mn dv Equation of state for ideal gas: r/ sin 2 θ = const. w B = p B = B2 2µ 0 = p + other forces = nqe + v B) p + other forces ρ m dv Condition for frozen-in magnetic field: Ohm s law: Conductivities: j = Cyclotron frequency gyrofrequency): = j B p + other forces n t + nv) = Q L p = nkt E + v B = 0 σ P σ H 0 σ H σ P 0 0 0 σ σ P = ne ωciν i B σ H = ne B σ = ne 2 ω 2 ci +ν2 i ω 2 ci ω 2 ci +ν2 i 1 m iν i + 1 E 0 E ) + ωceνe ωce 2 +ν2 e ) ω2 ce ωce 2 +ν2 ) e m eν e f c = ω c /2π) = 1 qb 2π m 5

Magnetic moment of charged particle gyrating in magnetic field: µ = 1 2 mv2 /B Magnetic force on magnetic dipole: Drift motion due to general force F: F B = µ B Pitch angle: v F = F B qb 2 tan α = v /v Electrostatic potential from charge Q in a plasma: Φr) = Q e r/λd 4πɛ 0 r Debye length: Plasma frequency: Rocket thrust: Specific impulse: The rocket equation: λ D = ɛ0 KT ne 2 f p = ω p /2π) = 1 ne 2 2π ɛ 0 m e I sp = T = v e dm T m fuel g = v e/g v = gt burn + v e ln 1 + m fuel m payload+structure ) Emitted thermal radiation power: Absorbed solar radiation power: P e = εσa e T 4 P a = αa a I rad 6