Perpendicular Flow Separation in a Magnetized Counterstreaming Plasma: Application to the Dust Plume of Enceladus

Similar documents
Simulation of the plasma environment of Titan in the magnetosheath flow of Saturn

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

Three-dimensional multi-fluid simulations of Pluto s magnetosphere: A comparison to 3D hybrid simulations

Mars as a comet: Solar wind interaction on a large scale

Kinetic effects on ion escape at Mars and Venus: Hybrid modeling studies

SW103: Lecture 2. Magnetohydrodynamics and MHD models

Introduction to the Sun-Earth system Steve Milan

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

David versus Goliath 1

8.2.2 Rudiments of the acceleration of particles

Introduction to the Sun and the Sun-Earth System

Chapter 8 Geospace 1

ELECTROHYDRODYNAMICS IN DUSTY AND DIRTY PLASMAS

Solar&wind+magnetosphere&coupling&via&magnetic&reconnection&likely&becomes& less&efficient&the&further&a&planetary&magnetosphere&is&from&the&sun& &

Hybrid Simulations: Numerical Details and Current Applications

Plasma Physics for Astrophysics

Modification of Titan s ion tail and the Kronian magnetosphere: Coupled magnetospheric simulations

Titan at the edge: 1. Titan s interaction with Saturn s magnetosphere in the prenoon sector

Titan s induced magnetosphere

Nonlinear MHD waves and discontinuities in the Martian magnetosheath. Observations and 2D bi-ion MHD simulations

Consequences of negative ions for Titan s plasma interaction

Dissipation Mechanism in 3D Magnetic Reconnection

Cold ionospheric plasma in Titan s magnetotail

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

Hybrid modeling of plasmas

A Multi-ion Model of the Heliosphere with Secondary Charge Exchange

THE PLASMA ENVIRONMENT OF COMET 67P/CHURYUMOV-GERASIMENKO THROUGHOUT THE ROSETTA MAIN MISSION

The Structure and Properties of Martian Magnetosphere at ~ 70 Solar-Zenith Angle in MSE Coordinates as Observed on MAVEN

Plasma interaction at Io and Europa

PARTICLE ACCELERATION AT COMETS

Recapitulation: Questions on Chaps. 1 and 2 #A

Interstellar Neutral Atoms and Their Journey Through the Heliosphere Elena Moise

Planetary Magnetospheres

Expansion of a plasma cloud into the solar. wind

Intro to magnetosphere (Chap. 8) Schematic of Bow Shock and Foreshock. Flow around planetary magnetic field obstacle. Homework #3 posted

Planetary magnetospheres

Basic plasma physics

OUR INTERCONNECTED PLANET

Magnetic Reconnection in Space Plasmas

The Magnetic Sun. CESAR s Booklet

Earth s Magnetosphere

MHD RELATED TO 2-FLUID THEORY, KINETIC THEORY AND MAGANETIC RECONNECTION

Asymmetric Magnetic Reconnection in Coronal Mass Ejection Current Sheets

Model investigation of the influence of the crustal magnetic field on the oxygen ion distribution in the near Martian tail

Numerical Simulation of Jovian and Kronian Magnetospheric Configuration

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

Planetary magnetospheres

Computational Plasma Physics in the Solar System and Beyond. Ofer Cohen HPC Day 2017 at UMass Dartmouth

High-latitude Bow Shock: Tilt Angle Effects

Macroscopic plasma description

Surprises from Saturn - and implications for other environments

Fran Bagenal University of Colorado

Titan at the edge: 2. A global simulation of Titan exiting and reentering Saturn s magnetosphere at 13:16 Saturn local time

Improved Hybrid Simulation on the Plasma Interaction of Titan

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.

Electromagnetic Fields in Space

Joseph Westlake and the PIMS Team OPAG: 24 August 2015

SOLAR WIND ION AND ELECTRON DISTRIBUTION FUNCTIONS AND THE TRANSITION FROM FLUID TO KINETIC BEHAVIOR

Magnetic Reconnection in ICME Sheath

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

2.A Material sources of gas and plasma

Morphology of the magnetic field near Titan: Hybrid model study of the Cassini T9 flyby

Interstellar and Interplanetary Material. HST Astrobiology Workshop: May 5-9, 2002 P.C. Frisch University of Chicago

Stability of the High-Latitude Reconnection Site for Steady. Lockheed Martin Advanced Technology Center, Palo Alto, CA

26. Non-linear effects in plasma

Real-time 3-D hybrid simulation of Titan s plasma interaction during a solar wind excursion

Plasma properties at the Voyager 1 crossing of the heliopause

Plasma collisions and conductivity

Three-fluid Ohm s law

A NEW MODEL FOR REALISTIC 3-D SIMULATIONS OF SOLAR ENERGETIC PARTICLE EVENTS

Magnetic Reconnection

A global model of cometary tail disconnection events triggered by solar wind magnetic variations

MHD Flow Field and Momentum Transfer Process of Magneto-Plasma Sail

Plasma environment in the wake of Titan from hybrid simulation: A case study

3D global multi-species Hall-MHD simulation of the Cassini T9 flyby

Magnetic Effects Change Our View of the Heliosheath

Solar-Wind/Magnetosphere Coupling

The chiming of Saturn s magnetosphere at planetary periods

From Sun to Earth and beyond, The plasma universe

Survey of the Solar System. The Sun Giant Planets Terrestrial Planets Minor Planets Satellite/Ring Systems

Titan s near magnetotail from magnetic field and electron plasma observations and modeling: Cassini flybys TA, TB, and T3

Alfvén Wings in the Lunar Wake: The

processes from studies of other magnetospheres

Dynamics of the Jovian magnetosphere for northward interplanetary magnetic field (IMF)

1.060 Engineering Mechanics II Spring Problem Set 3

Physics of the Ion Composition Boundary: a comparative 3-D hybrid simulation study of Mars and Titan

Planetary Magnetospheres: Homework Problems

X-ray imaging of the magnetosphere

A Comparison between the Two-fluid Plasma Model and Hall-MHD for Captured Physics and Computational Effort 1

The Dynamic Magnetosphere. Ioannis A. Daglis. National Observatory of Athens, Greece

Interstellar Medium V1

Lecture 5 The Formation and Evolution of CIRS

Hall effect in the coma of 67P/Churyumov Gerasimenko

Phase-standing whistler fluctuations detected by SELENE and ARTEMIS around the Moon

Explain how the sun converts matter into energy in its core. Describe the three layers of the sun s atmosphere.

MHD simulation of solar wind using solar photospheric magnetic field data

What do we see on the face of the Sun? Lecture 3: The solar atmosphere

Mechanisms for particle heating in flares

LABORATORY SIMULATION OF MAGNETOSPHERIC PLASMA SHOCKS

Modeling and Simulating Flowing Plasmas and Related Phenomena

Transcription:

Perpendicular Flow Separation in a Magnetized Counterstreaming Plasma: Application to the Dust Plume of Enceladus Y.-D. Jia, Y. J. Ma, C.T. Russell, G. Toth, T.I. Gombosi, M.K. Dougherty Magnetospheres of the Outer Planets 1600, Monday, July 11, 2011 Boston, Massachusetts 1

Introduction Charged dust is widely observed in space plasmas In this talk we show how charged dust disturbs the surrounding plasma flow We start with the basic physics of plasma charged dust interaction in a spherical dust cloud and then apply it to the Enceladus environment The dust is treated as a fluid while the charging process is neglected 2

The importance of mass ratios The behavior of an electron-positron plasma is much different than the behavior of an electron-proton plasma Two key processes in heliospheric plasmas where the size of the mass ratio matters are collisionless shocks and collisionless magnetic reconnection Heating of electrons and ions is quite different in shocks Magnetic field line breaking requires electron scale anisotropies Not much work has been done on situations in which there is a third very different mass ratio but this situation occurs frequently in the heliospheric plasma Cometary and atmospheric ion pickup such as SO 2 + at Io AMPTE Barium release Cometary dust, interplanetary dust and Enceladus plume interactions This pickup is now generally handled with hybrid simulations. Can we adapt MHD codes to handle charged fluids with quite different mass ratios? 3

Charged dust in the solar wind: Coordinate system B z y Dust We illustrate this problem with a simple magnetized solar wind (electron-proton) flow interaction with charged dust Dust particles are loaded as a spherically symmetric cloud at the origin The red arrows mark the directions of Lorentz forces q(e+v B) of the positively charged dust case. The simulation uses the multi-fluid MHD code, BATSRUS E x F i + F D + 4

The multi-fluid MHD equations The conservation equations of the ion and dust fluids, as represented by s : Mass Momentum Faraday s Law Energy 5

Flow Separation Along the Connection Electric Field The convection of magnetic field follows the charge-averaged velocity From this definition we can deduce the Lorentz forces on the ion and dust fluids: Positively charged dust: Negatively charged dust: Instead of E B drifting, the dust is massive enough to ignore the magnetic field and thus both fluids move along the Lorentz forces above. Such flow separation has been understood for decades, but the field perturbation was missed Along the convection electric field, the ions and dust move oppositely to maintain the original zero momentum. However, the electrons follow the combined motion of these heavy charges, which is different from the motion of the momentum center. This difference, causes the pileup of field in the perpendicular direction. 6

Positive charge Negative charge Charged dust in the solar wind: Signs of dust charge Density-field lines Density-stream lines current Ion velocity e f g h 7

Parameters along a line cut Positive charge Negative charge 8

The 3-D structure of the plasma tail: Positively charged dust case A standard plasma tail of an active comet lies along the x-axis with currents flowing along z (left sketch). Not only the ion tail caused by dust pickup is shifted towards +z, but also its current is rotated towards x (right figure). Modeled tail current sheet Standard cometary tail current sheet that closes around the tail lobe. Z Y X Blue: current density isosurface J=0.02 A/m 2 9

Dust interactions at Enceladus: Change of geometry y To Saturn E F D - F i - B Dust x 10

Negatively charged dust at Enceladus: Simulation results 11

Magnetic field Current system in 3-D Both the field contour and the Alfven wing current system are rotated counterclockwise. Both northern and southern wings are also pushed anti-saturnward. The rotation is consistent with the Cassini By observation that was not explained with single fluid models. Positively charged dust rotates the system clockwise and pushes both Alfven wings Saturnward. Iso-surface of total current density J=0.02 A/m 2 To ionosphere To ionosphere Single fluid mass loading gas (stronger momentum loading rate) Multi fluid with negatively charged 12 dust

Summary The model reproduces the expected plasma deceleration with both positively charged and negatively charged dust, but a new effect arises. Negatively charged dust causes the magnetic field to bend in the direction of the convection electric field, while positively charged dust causes the opposite magnetic field bending. Consequently, the interaction does not only result in a perpendicular shift in the disturbed region, but also a rotation of disturbed field towards or against the convection electric field. We find that the same perpendicular bending exists for all counterstreaming interaction problems, independent of the shape of the dust cloud. The anti-hall effect that was introduced in a previous study ignores the resulting anti-saturnward flow, can not predict the shift in the Alfven wings, and limits its application. Our model can be applied to plasma interaction studies including, but not limited to, charged dust particles in the solar wind, cometary plasma, the Enceladus plume, and active plasma releases, such as the Active Magnetospheric Particle Tracer Experiment (AMPTE) mission. The predicted behavior is consistent with observations at Enceladus. 13

Backup slide 14

Difference from the Anti-Hall effect Simon et al. [2011] introduced the Anti-Hall effect to explain the dust-plasma interaction at Enceladus. In their treatment, the electron bulk velocity is assumed to be the upstream bulk plasma velocity: In a multi-fluid description, the electrons have their own velocity, and they are decelerated because of the draping field. Thus Simon et al. [2011] requires a critical charge density of the dust particles for the Anti-Hall effect to apply: The fundamental multi-fluid MHD theory does not restrict such perpendicular field bending to any relative density conditions. Instead, such bending exists in any heavy ionplasma interaction. 15