Title: Solar wind interaction with the comet Halley and Venus
1Solar wind interaction with the comet Halley and
Venus
- K. Murawski
- University of M. Curie Sklodowska
2 Outline
- Overview of solar wind interaction with
- magnetic and non-magnetic bodies
- Numerical simulations of the solar wind
- interaction with Venus
- Numerical simulations of the solar wind
- interaction with the comet Halley
- Summary
3 A global view of the Heliosphere
4Solar system - Icy Matter ...
Jan Oorts Cometary Cloud
5Outskirts of the Solar system - Comets
6Properties of the solar wind
- highly conducting plasma
- electrons, protons alpha-particles
- radial expansion
- magnetic field frozen in the plasma
- SW super-sonic super-alfvénic
- ne 5 cm-3
- T 105 K
- BIMF 5 nT
- vsw 400 km/s
- vA 30 - 50 km/s
- cS 60 km/s
7TYPES OF INTERACTION WITH THE SOLAR WIND
GANIMEDE
8Simplest caseEarth's MOONNO magnetic fieldNO
atmosphere
9MOON type
- no magnetic field
- negligibly thin atmosphere
- insulating material
- submerged in a flowing plasma
- absorption of particles
- no bow shock upstream
- plasma absorption wake
- magnetic field parallel to the upstream flow ? no
effect - magnetic field perpendicular to the flow ?
minimal effect
Illustration of the interplanetary plasma flow
and magnetic-field perturbation by the
nonconducting moon. The wake created by
solar-wind absorption closes more quickly when
the magnetic field is not aligned with the
undisturbed flow.
10SW interactions with magnetized bodiesand an
atmosphere
Obstacle magnetosphere
11EARTH type (Jupiter, Saturn)
- strong magnetic field
- substantial atmosphere
12SW interactions with magnetized bodiesbut
without an atmosphere
Obstacle magnetosphere
13MERCURY - type
- strong magnetic field
- no gravitationally bound atmosphere
- Similarities and differences with Earth
- Magnetosphere
- Absence of an atmosphere and ionosphere
- Solar wind conditions
- Mercury has a larger fractional volume of its
magnetosphere - no stable trapping regions
- closed magnetic flux tubes
- Solar wind primary source of magnetospheric
plasma - Plasma sheet higher densities
0.382 AU Mercury
14COMETSNO internal magnetic fieldbut atmosphere
Obstacle exosphere
15What is Solar Wind?
16Comet Structure
- Nucleus main solid core of the comet.
- Tail gas and dust particles released by the
comet. - Coma gases and dust released by the comet when
energy from the sun heats the comet and causes
the solid materials to turn into a gas.
17Comet Tails
- Comets develop tails only when the get close
enough to the Sun. - Comet tails always point away from the SunThis
is how scientists first realized the existence of
solar wind.
18Comet type
- no internal magnetic field
- substantial atmosphere
19 20 21 22 23 24 25 26SW interactions with unmagnetized bodies with a
substantial atmosphere
Obstacle ionosphere
27Venus
28VENUS type
- weak magnetic field or non at all
- substantial atmosphere
29Structure of the Ionosphere
Brace and Kliore, 1991
30Location of the obstacle boundary
31Induced magnetotail
32Pick up and escape processes
Escape
Energetic neutral atoms (ENAs)
Escape
33Ionospheric magnetic field
34(No Transcript)
35Altitude (Km)
Number Density (cm-3)
36Numerical model - Draping magnetic field lines
Solar wind
37Physical model 2 component MHD
38Parameters of the physical model
39Pressure distribution
Interaction region
IMF
bow shock
magnetic barrier
ionosphere
40Pressure profiles in the subsolar region
X
41Plasma profiles
X
42Magnetic field lines and nightside ionosphere
Z
XZ plane
Solar wind
X
IMF
Y
XY plane
43Concluding remarks
- Flowing plasma interactions with various types of
- magnetized planets or
- unmagnetized / weakly magnetized bodies
- Each plasma interaction has distinctive features
- Earth magnetic field and atmosphere
- Mercury magnetic field but NO atmosphere
- Moon like bodies neither a magnetic field nor
an atmosphere - Venus and Mars no internal magnetic field but
a substantial atmosphere - Comets atmospheres with insignificant bodies
44Thank you!
kmur_at_kft.umcs.lublin.pl