The effects of the solar wind on Saturn’s space environment

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Presentation transcript:

The effects of the solar wind on Saturn’s space environment A. Masters1 On behalf of the Cassini science community 1Imperial College London, UK

Outline The solar wind – a space plasma Saturn’s magnetosphere Cassini’s exploration of the magnetosphere How the solar wind affects the magnetosphere: - Size of the magnetosphere - Auroral emissions - Reconnection - Waves in the outer magnetosphere Summary NASA/JPL

The solar wind The Sun is made of partially ionized gas – a plasma (charged particles not bound together as atoms or molecules) There is a large pressure difference between the surface of the Sun and the outer solar system As a result the particles of the solar surface flow away from the Sun All the planets are immersed in this solar wind, like pebbles in a stream Credit: F. Espenak (NASA/GSFC ) Low pressure outer solar system Solar wind Sun High pressure solar surface Saturn’s orbit

What is special about space plasmas? Space plasmas (like the solar wind) are very low density, a better vacuum than we can make in a laboratory Because of their low density, magnetic field lines threading a space plasma are ‘frozen-in’ → Wherever the plasma goes the magnetic field lines have to go too → Two different space plasmas with different frozen-in magnetic fields cannot mix Magnetic field lines Magnetic field lines Space plasma 1 Space plasma 2 No mixing

What does the solar wind do to the Sun’s magnetic field? The Sun generates its own magnetic field As the solar wind flows away from the Sun it carries this magnetic field out into the solar system This solar wind magnetic field is called the interplanetary magnetic field (IMF) Due to the Sun’s rotation, the IMF field lines extending out into the solar system form a spiral pattern – The famous Parker spiral Solar wind flow Sun Interplanetary magnetic field lines Rotation of the Sun

The Saturn system NASA/JPL

Saturn’s magnetic field www.school-for-champions.com/science/magnetic_detection.htm Saturn’s magnetic field Saturn generates a magnetic field (like the Earth) due to processes operating in the planet’s interior Saturn’s rotation North pole Magnetic field lines N S The field is dipolar – like the field of a bar magnet Saturn’s magnetic axis and spin axis are closely aligned South pole

Saturn’s magnetosphere Solar wind flow Planetary magnetic field lines N Sun Solar wind flow S Solar wind flow The plasma around Saturn is frozen-in to the planet’s magnetic field, the solar wind plasma is frozen-in to the IMF → the two cannot mix, Saturn’s field is an obstacle to the solar wind

Saturn’s magnetosphere Bow shock N The solar wind flows at ~500 km/s This high speed means that the only way to slow the solar wind down so it can flow around Saturn’s magnetic field is via a shock wave, called the bow shock (analogous to the shock waves seen in front of supersonic aircraft) S

Saturn’s magnetosphere Downstream of the bow shock the solar wind is slower, hotter, and denser, and the plasma flows around the planetary field obstacle This region is called the magnetosheath S Magnetosheath

Saturn’s magnetosphere The boundary of the planetary field obstacle is called the magnetopause Generally, solar wind plasma cannot flow across this surface The position of the magnetopause corresponds to pressure balance between the solar wind and the planetary field S Magnetopause

Saturn’s magnetosphere The region where the Saturn’s magnetic field is experienced is called the magnetosphere On the planet’s sunward side the field is compressed S Magnetosphere

Saturn’s magnetosphere Magnetotail S On the antisunward side of the planet, the field lines extend to form a long magnetotail

The solar wind-magnetosphere interaction: why study it? As we will see in the following slides, the solar wind can profoundly affect Saturn’s magnetosphere To better understand the physics of Saturn’s magnetosphere it is essential that we study the solar wind-magnetosphere interaction Compared to the equivalent interaction at Earth and at Jupiter, the Saturn interaction is different in many respects By examining the interaction at Saturn we may learn something new about how the solar wind interacts with other planets

Cassini’s approach to the Saturn During Cassini’s approach to Saturn we were able to observe many of the properties of the solar wind 10 times further from the Sun than the Earth Hubble Space Telescope images of the planet allowed us to study the effect of changing solar wind conditions Taken from Matson et al. [2002]

Cassini’s exploration of the magnetosphere Since arriving at Saturn in July 2004 Cassini has spent a significant amount of time within the planet’s magnetosphere By the end of the mission the spacecraft will have comprehensively explored Saturn’s space environment Sun Dawn side N S Dayside Nightside Sun Sun Dusk side

Solar wind at Saturn orbit Taken from Jackman et al. [2004] Solar wind at Saturn orbit Cassini observations made during the spacecraft’s approach to Saturn revealed that the solar wind consisted of alternating regions of compression (higher density) and rarefaction (lower density) rarefaction rarefaction Saturn’s magnetosphere compression compression rarefaction compression rarefaction

Size of the magnetosphere These compressions and rarefactions resulted in changes in the total pressure exerted by the solar wind on the magnetosphere → Motion of the magnetopause to maintain pressure balance Due to such solar wind variations the magnetosphere can dramatically expand/contract This has a clear effect on other magnetospheric phenomena Range of magnetopause positions Sun Sun Crossings normalized to the same solar wind pressure Taken from Arridge et al. [2006]

Solar wind influence on auroral emissions Like Earth, Saturn has aurorae These emissions are caused by charged particles that travel along magnetic field lines and hit the planet’s upper atmosphere Saturn Earth http://hubblesite.org/ www.destination360.com/north-america/us/alaska/aurora-borealis.php/

The ultraviolet aurorae rarefaction compression Taken from Crary et al. [2005]

Saturn kilometric radiation Saturn’s mysterious auroral radio emission is called Saturn kilometric radiation (SKR) Taken from Cecconi et al. [2009] Intense SKR associated with a compression of the magnetosphere The SKR power varies with a variable period close to the rotation rate of the planet – the solar wind also affects this modulation period Taken from Bunce et al. [2005]

Reconnection Magnetic reconnection is a particularly important process that can operate in space plasmas Simple picture: Anti-parallel field lines break, and reconnect The process energizes the plasma and is important for our understanding of planetary magnetospheres Magnetic field 1 Magnetic field 2 Reconnected field lines Plasma flow

Dayside reconnection Sun Sun Sun The IMF field lines carried by the solar wind can reconnect with Saturn’s magnetic field lines, particularly when the IMF points North → entry of solar wind plasma into the magnetosphere Cassini has found evidence of reconnection at the magnetopause; however the nature of dayside reconnection at Saturn appears to be different to that at Earth and Jupiter Reconnected field lines pulled over the poles by the solar wind flow IMF Planetary field N N N Reconnected field lines S S S Sun Sun Sun

Magnetotail reconnection Evidence for reconnection in the magnetotail has been found by Cassini and is linked to intense auroral emissions and the generation of energetic neutrals It has been suggested that rapid bursts of tail reconnection are triggered by solar wind-induced compression of the magnetosphere Do Earth-like substorms occur at Saturn? Planetary field (in the magnetotail) Reconnected field lines Anti-parallel field N N N S S S Plasma flow Sun Sun Sun

Waves on the magnetopause Dawn flank Solar wind pressure fluctuations can produce waves on the magnetopause surface When the plasma flows either side of the boundary are very different, waves can also be generated due to the growth of the Kelvin-Helmholtz (K-H) instability This is analogous to waves on the sea caused by wind blowing across the surface Magnetospheric flow Solar wind flow Dusk flank Magnetopause v1 Magnetopause v2 time

Waves on the magnetopause Cassini has found evidence of complicated wave structures on the magnetopause surface, likely driven by the K-H instability These waves are expected to launch more waves into the magnetosphere itself, leading to energy transport Saturn Magnetopause Magnified view of the boundary Taken from Masters et al. [2009] Taken from Cramm et al. [1998]

Summary The interaction between the solar wind and Saturn’s magnetic field produces a cavity around the planet – the magnetosphere This space environment is complex and can be significantly affected by changes in the solar wind In many ways, this interaction at Saturn is different from the interaction at the other planets of the solar system Cassini’s ongoing exploration of near-Saturn space should further improve our understanding of the environment