- Open Access
The orientation of Titan’s dayside ionosphere and its effects on Titan’s plasma interaction
© The Society of Geomagnetism and Earth, Planetary and Space Sciences (SGEPSS); The Seismological Society of Japan; The Volcanological Society of Japan; The Geodetic Society of Japan; The Japanese Society for Planetary Sciences; TERRAPUB. 2012
- Received: 16 March 2011
- Accepted: 3 August 2011
- Published: 8 March 2012
A hybrid particle code has been used to examine how Titan’s interaction with Saturn’s magnetosphere is effected by the orientation of the dayside ionosphere with respect to the incident magnetospheric flow. The hybrid code self-consistently includes a version of Titan’s ionosphere represented by 7 generic ion species, over 40 ionneutral chemical reactions, ion-neutral collisions and Hall and Pederson conductivities. Emphasis is placed on what effects the orientation angle has on the ion loss rates, ion densities, and the electric and magnetic fields. The results are analyzed and regardless of the orientation angle the ionosphere is found to be within photochemical equilibrium below 1200 km altitude. The ion loss rates and field structures also show little dependence on the orientation of the dayside ionosphere. It is found to first order illumination angle does not have a significant effect on these features of the Titan interaction.
- plasma interaction with Saturn’s magnetosphere
Understanding the dynamics of Titan’s plasma interaction and how its ionosphere couples to Saturn’s magnetosphere is a complex problem. Full 3-dimensional simulations that include accurate descriptions of the plasma, the ionospheric chemistry and the neutral atmosphere are a critical tool to help solve the problem. This paper presents results from 3-d hybrid (kinetic ions, fluid electrons) simulations of Titan’s plasma interaction that include ionospheric chemistry, ion-neutral and electron-neutral interactions.
The first in-situ observations of Titan’s interaction region were made by a single flyby of Voyager 1 through Titan’s wake in 1980. No intrinsic magnetic field was found at Titan (Ness et al., 1982). Titan was found to have an extensive ionosphere that interacts directly with Saturn’s magnetospheric plasma and fields (Hartle et al., 1982; Bird et al., 1997). The interaction leads to Saturn’s magnetic field piling up and draping around Titan forming an induced magnetosphere (Ness et al., 1982). Voyager also observed Titan’s ionospheric ions being lost to Saturn’s magnetosphere (Hartle et al., 1982). Net ion loss rates were estimated to be 1−3 × 1024 ions/s (Eviatar et al., 1982; Gurnett et al., 1982).
After the first Titan encounter it was speculated that Titan’s interaction with Saturn’s magnetosphere could be more complex than the Voyager picture. Unlike the solar wind’s interaction with the planets, Titan’s interaction with Saturn’s magnetospheric flow does not have to coincide with the solar produced ionosphere. While the planets only interact with the solar wind, Titan can be found in Saturn’s magnetosheath, tail, or in the flanks of the planet. These different orientations lead to different plasma conditions at Titan (cf. Wolf and Neubauer, 1982; Cravens et al., 1998; Ledvina and Cravens, 1998; Ledvina et al., 2004a; Bertucci et al., 2009; Rymer et al., 2009).
Cassini spacecraft made its first flybys of Titan in 2004. Since then Cassini has made over 76 flybys of Titan. Cassini has confirmed many of the previous Voyager results such as the lack on an intrinsic magnetic field and an induced magnetosphere (Backes et al., 2005). However, Cassini has also found the Titan interaction to be even more variable and complex than previously thought. The ionosphere contained several species with mass greater than 100 amu (Waite et al., 2005) as well as negative ions (Coates et al., 2007). A substantial night side ionosphere was found (Wahlund et al., 2005; Cravens et al., 2006; Ågren et al., 2007, 2009). There has been some debate over the source of the night side ionosphere. The short lived ions in the night side ionosphere may be created by super thermal electron impact ionization (Gan et al., 1992; Ågren et al., 2007; Cravens et al., 2009), while plasma transport from the day side to the night side of the long lived ion species may also occur (Cui et al., 2009).
Cassini made the first measurements of Titan’s ionospheric conductivities (Rosenqvist et al., 2009). The peak Hall and Pederson conductivities were found to be dependent on the solar illumination and the magnetospheric conditions. The conductivities were typically higher on the sunlit side but depended strongly on the magnetic field magnitude and the field draping configuration. A consistent double peak was found in the altitude profile of the Pederson conductivity. The first peak was within 1300–1400 km altitude. The second peak was located below 1000 km, were the magnetic field strength drops sharply but the electron density is still high. The Pedersen conductance was always found to be higher than the local Alfvén conductance (from a factor of 4 to 100 times greater). The Pederson conductivity profile should give rise to complicated ionospheric-atmospheric dynamics. It also implies that the conditions for the ionosphere to reflect or absorb Alfven waves are highly variable and strongly dependent on the magnetic field strength (Rosenqvist et al., 2009).
Recently Ågren et al. (2011) combined data from radio and plasma wave science, the magnetometer, the plasma spectrometer with the ionospheric conductivities. They found currents flowing in Titan’s ionosphere ranging from 10–100 nA/m2. Below altitudes of 1400 km (the exobase) the currents were principally field aligned (Hall), the Pederson currents were found to be negligible. Perpendicular electric fields ranging from 0.5–3 μV/m were associated with the observed currents.
The plasma and field conditions along Titan’s orbit have been found by Cassini to be more variable than previously thought (cf. Bertucci et al., 2009). This variability was found to be crucial to understanding aspects of the T9 observations by Modolo et al. (2007). After the Voyager encounter the magnetic field was thought to be nearly perpendicular to Titan’s orbital plane throughout the orbit. Cassini has found this to be the exception rather than the rule. Arridge et al. (2007) has interpreted Cassini magnetometer observations as a thin current sheet in the form of a magnetodisc. A follow up study by Arridge et al. (2008) found that the magnetodisc, and hence Saturn’s magnetosphere, is strongly influenced by solar wind dynamic pressure. The magnetodisc is warped by the solar wind. This warping exposes Titan to quasi-dipolar fields in the noon sector and planet-ward, swept-back fields in the dawn, dusk and midnight sectors. Depending on where Titan is in relationship to the magnetodisc it is exposed to either: (1) a ‘magnetodisc lobe’ regime where the plasma beta is low and fields are radially ‘stretched’ and usually stronger or (2) a ‘current sheet’ regime characterized by quasi-dipolar, relatively weak fields and a high-beta plasma (Bertucci et al., 2009).
Additional studies of electron density in the magnetodisc have found that periodicity in the magnetosphere are due to plasma outflows driven by centrifugal force. This material originates from Enceladus and works its way out to Titan. This periodicity can cause a larger variability at Titan than the solar wind (cf. Persoon et al., 2005, 2006; Morooka et al., 2009).
Simon et al. (2010a) classified the first 62 Titan flybys as lobe-type or current sheet. They concluded that not a single flyby up to then matched the Voyager picture of a homogeneous background magnetic field perpendicular to the moon’s orbital plane. The magnetic field varied on time scales ranging from a few minutes to several hours. These observations were later verified in a follow up study using data collected along Titan’s orbit when Titan was not present (Simon et al., 2010b). To further complicate things there are times when Titan has been observed within Saturn’s magnetosheath (cf. Bertucci et al., 2008; Garnier et al., 2009). Understanding the magnetospheric variability is crucial to understanding Titan’s interaction. Asymmetries in the observed ion densities and composition downstream of Titan during the T9 flyby were attributed by Modolo et al. (2007) as being due to the variability in the magnetic field morphology.
Interpretations of the Voyager PLS data found a two component plasma consisting of H+ and N+ with number densities of 0.1 and 0.2 cm−3 respectively. Both species were found to have gyroradii comparable to Titan (1RT = 2575 km). Each species was fitted with a Maxwellian distribution function with a thermal speed of 200 km/s (Hartle et al., 1982). It was suggested by Eviatar et al. (1982) that the N+ originated from Titan and formed a torus about its orbit. Based on the assumption that the N+ component could be pickup ions, Ledvina et al. (2005) showed that the PLS data could be fit by a shell distribution. The post Cassini picture has found that the N+ component was really O+ and is thought to originate from the icy satellites and moons (Szego et al., 2005). Szego et al. (2005) fit the incident O+ to a shell distribution function. The Cassini plasma data along Titan’s orbit have been fit to Maxwellian, shell and kappa distribution functions. The exact distribution function of the incident plasma is still an issue that remains to be settled.
Simulations have been used over the years to understand Titan’s interaction with Saturn’s magnetosphere. Initial 1-D simulations included single and multifluid MHD and hydrodynamics were used to predict the magnetic flux into the ionosphere and ion loss out the tail (e.g., Ip, 1990; Keller and Cravens, 1994; Keller et al., 1994). These simple 1-D simulations were followed by a multispecies 2-D MHD model (Cravens et al., 1998) and a single fluid MHD model (Ledvina and Cravens, 1998). These early multidimensional simulations confirmed the basic post-Voyager picture of Titan’s interaction but they did not have a realistic ionosphere. Higher resolution MHD studies followed (Kabin et al., 1999; Kopp and Ip, 2001; Nagy et al., 2001; Ma et al., 2004, 2006, 2007; Backes et al., 2005) as did a multifluid simulation by Snowden et al. (2007). The later studies by Ma et al., were multispecies (7 continuity equations) but single fluid (1 momentum equation), they included ion-neutral collisions and chemistry. Their latest results Ma et al. (2007) also include the Hall term in the MHD equations.
These simulations have been successful at describing many aspects of Titan’s plasma interaction. However, they are all based on the fluid approximation. Gyroradius effects and none isotropic pressures are not described in this approximation. The fluid approximation cannot provide a complete description of the interaction because of the size of the ion gyroradii near Titan. This issue was recognized early on with initial studies of the kinetic effects being carried out by particle tracing in ideal and MHD fields (cf. Luhmann, 1996; Ledvina et al., 2000, 2004b, 2005; Tseng et al., 2008). Particle tracing gives a better sense of the importance of gyroradius effects than MHD simulations but it is not self-consistent. There is no feedback between the particle motion and the fields. Self-consistent hybrid simulations (kinetic ions, fluid electrons) have been carried to account for the ion gyroradii effects near Titan (e.g. Brecht et al., 2000; Ledvina et al., 2004a; Sillanpää et al., 2006; Simon et al., 2006; Modolo et al., 2007; Müller et al., 2010). The major limitation to the hybrid simulation performed to date has been their lack of any description of the ionosphere.
The research reported here addresses this limitation in the previous hybrid simulations. We have applied our experience from incorporating ionospheric processes into hybrid simulations of Mars (cf. Brecht and Ledvina, 2012) to Titan. The resulting ionosphere contains seven generic ion species and the same ion-neutral chemistry used by Ma et al. in their Titan simulations. There are eleven neutral species whose altitude profiles are based on Cassini observations and the model of Toublanc et al. (1995). The ions not only interact with the neutrals chemically but also through collisions via their respective collisional cross sections. The ion-neutral collision process is also used to self-consistently include the Hall and Pederson conductivities into the electric field calculation. Photoionization on the dayside is the major ionization source, but secondary electron impact ionization is also included. The night side ionosphere is created from superthermal electron impact ionization (cf. Gan et al., 1992; Galand et al., 1999; Ågren et al., 2007; Cravens et al., 2009). The effect of Titan’s gravity on the ion motion is also included.
Sillanpää et al. (2006) have previously examined the effect of the angle of solar illumination with respect to the incident flow. They concluded that the illumination angle did not make much of a difference with regard to the amount of plasma lost from Titan. Their results were cutting edge at the time. However, several simplifying assumptions were necessary so that the simulations could be performed. The inner boundary of their simulation was Titan’s exobase. This surface was modeled as a perfectly conducting sphere of radius 4175 km. They were only able to include two ion species. The first, N2+ was emitted uniformly from Titan’s exobase. The second, CH4+ was photoionized from a Chamberlain density function. They did not include any ionospheric processes in their simulations. Furthermore their simulations were limited to less than 2 million particles to represent both the magnetospheric and ionospheric plasmas. Given the complexity of Titan’s ionosphere and its importance as a boundary condition it is worth re-examining the effects of the illumination angle on ion loss from Titan.
The next section provides a discussion of the models used in the simulations. A discussion of the ion loss for each case follows. The last two sections will provide a discussion of the results and some conclusions.
2.1 The plasma model
The plasma is modeled using the hybrid approximation. The plasma is assumed to be charge-neutral. The ions are treated as kinetic particles, while the electrons are treated as a massless fluid. The displacement current is dropped from Maxwell’s equations by use of the Darwin approximation (cf. Brecht and Ledvina, 2006). This results in the removal of light waves from the simulation. However, a full set of electromagnetic waves up to and including the ion Whistler waves are retained. The quasi-neutrality assumption means that charge separation and electrostatic instabilities are also removed from the simulations. While the massless electron assumption means that high frequency modes due to the electron motion cannot be simulated. The lack of charge separation and m e means that scale sizes need to be much larger than the Debye length, the magnetic skin depth and the electron skin depth. Under these assumptions the resulting set of equations describes the plasma:
The electric field used in Eqs. (3) and (4) is found from Eq. (6). The electron current in Eq. (6) is found by subtracting the ion current obtained by the particles from the total current found with Eq. (2). The equations are solved using a predictor-corrector algorithm developed by Harned (1982). Further discussion about the hybrid approximation, solution algorithms and applications can be found in Ledvina et al. (2008) and references there in.
When the neutral densities become significant ion-neutral and electron neutral collisions will modify the electric field via the Hall and Pederson conductivities. These processes are important in Titan’s ionosphere and indeed the conductivities have been measured as mentioned above.
The quasi-neutrality condition (Eq. (1)) is the basis of any hybrid or MHD model. Strictly speaking it is not necessary for the electron density to be equal to the ion density only that the density of negative charge carriers equals the density of the positively charged carriers and charge separation not be allowed. At Titan n e = n i is a good approximation above 1200 km. However, below that altitude negatively charged massive ions have been found in Titan’s ionosphere (Coates et al., 2007). The mass distribution of the negative ions in Titan’s ionosphere was found to increase at low altitudes and at high latitudes. There was also a weak mass dependence on the solar zenith angle Coates et al. (2009). The creation and dynamics of the negative ions is not well understood and is a topic of current research. The simulation results presented here do not include a model for the negative ions.
The simulation are performed in Titan centered Cartesian coordinates extending ±10Rt in each direction. A cell size of 250 km is used to resolve the electric and magnetic fields. Chemistry and ion-neutral collisions are resolved on different grids and are described in the following subsections. Ions are injected upstream of Titan with a mass of 16 amu and a density of 0.2 cm−3. We take the simplest approach possible and load the upstream ions cold with an E × B drift speed of 120 km/s with respect to Titan. The incident magnetic field is 5 nT and is perpendicular to Titan’s orbital plane. Below an altitude of 1400 km the electron temperature profile is based on the Langmuir probe results (Ågren et al., 2009) and is held constant.
2.2 The neutral atmosphere model
The neutral atmosphere used in the simulations is assumed to be stationary, spherically symmetric and consist of 11 neutral species, H, H2, CH4, HCN, N2, C2H2, C2H4, C2H6, C3H4, C4H2 and HC3N. Of these species the density profiles of CH4 and N2 were taken from the INMS profiles during the TA encounter (Waite et al., 2005). The neutral profiles for the other species came from the model of Toublanc (cf. Keller et al., 1998; Toublanc et al., 1995).
2.3 The ionosphere
The generic ion species used in the model, the actual ion species they represent, their assigned mass and the mass range of the actual ions represented.
Titan’s lower ionosphere has been found to be dominated (between 10–60%) by heavy (greater than 100 amu) organic compounds (cf. Crary et al., 2009; Wahlund et al., 2009). These compounds are currently represented in our model by the HHC+ and HNI+ species. These species contain a representation of all the heavy and very heavy hydrocarbon and nitrile ion species and related chemistry. They provide a fair representation of this part of the ionosphere for the purposes of this study. The ionospheric model used in the simulations is an initial step that will be refined as understanding of Titan’s ionosphere improves. Further details about the model can be found in Appendix A.
The ion-neutral chemical model is implemented into the hybrid code using a spherical grid similar to the grid used for the neutral collisions described above. The density of each ion species is volumetrically weighted to the cell corners. The ion-neutral chemistry is then integrated explicitly. At the end of the integration time, 1 particle is added for each species in every cell of the chemistry grid. This particle is weighted such that it represents the total density created in that cell during the integration time. The weights of the old particles of a given species located in the cell are reduced to account for losses due to recombination and chemical reactions. At the start of each simulation the ion-neutral chemistry is evolved for 20000 s to ensure that chemical equilibrium is reached to an altitude of 2000 km. This is well above the altitude where the advection time scales are equal to the net ion production time scales. The ionosphere is over built at start up, it then erodes until a balance is reached between the rate the ions are produced and the rate they are being advected away. This approach avoids the potential problem of the ions being lost to Saturn’s magnetosphere before the ionosphere has a chance to build. Hence a fully developed ionosphere is present when the run begins. While the simulations are running the chemistry package is able to accurately respond to changes in the ion densities.
The plasma and field conditions are the same for each case. The magnetic field is taken to be 5 nT pointing southward perpendicular to Titan’s orbital plane. We take the incident plasma to consist of only O+ with a density of 0.2 cm−3 moving with a speed of 120 km/s with respect to Titan. The incident electrons have a density of 0.2 cm−3 and a temperature of 200 eV. We do not address the issue of the upstream ion distribution function but adopt the simplest approach and load the ions with a beam distribution.
4.1 Ion loss rates
There are two straightforward questions that the simulation results can be used to answer. The first is how much of each ion species is Titan losing to Saturn’s magnetosphere? The second is does the orientation of the sun with respect to the plasma flow direction effect those loss rates? To address these question we constructed a 5Rt sampling box centered on Titan. Ions that crossed the sampling faces where collected over the time of each run and recorded. The loss rates were then calculated. Each simulation was run until the loss rates became stable. All of the cases took longer than 2700 s of simulation time (not run time) for the loss rates to stabilize. Rates collected before that time overestimated the loss of L+ and M+. All of the species except the HNI+ (74 amu) first hit the sampling box within 500 seconds, with L+, M+, H1+ and H2+ all hitting in less than 100 s. The MHC+ first hit the box around 250 s while the HHC+ took almost 500 s. The HNI+ took more than twice as long, over 1300 s to reach the box. The lower the altitude of the peak density for a given species, the longer it takes that species to escape and be sampled at 2.5Rt.
The net ion loss rates for each species.
3.0 × 1021
3.0 × 1021
2.3 × 1021
1.7 × 1024
1.7 × 1024
1.5 × 1024
3.0 × 1024
3.2 × 1024
1.9 × 1024
7.0 × 1023
6.9 × 1023
6.4 × 1023
2.8 × 1023
2.7 × 1023
2.7 × 1023
5.7 × 1022
6.1 × 1022
6.6 × 1022
2.0 × 1019
9.1 × 1019
1.2 × 1019
Figure 7 shows the loss rate as a function of the species mass for each case. The altitude of the dayside ionospheric density peak for each species is also plotted. The loss rates for a given species are fairly consistent. For most of the masses case 2 is the orientation that leads to the largest ion escape, though only slightly. There is also an altitude trend for most of the masses. The more massive the species, the lower the altitude of its ionospheric density peak and the lower its loss rate to Saturn’s magnetosphere is. The exception to that trend is the L+ species. It’s interesting to note that the loss rates for the H1+ and H2+ are different even though their masses are about the same (29 versus 28 amu). They should respond to the electric and magnetic fields in a very similar fashion. So the expectation that their loss rates should be similar would not be unreasonable. They are not shown here but the particle trajectories for each species outside of the ionosphere are very similar. The difference in their loss rates is a result of their creation. The ion density profiles in Fig. 3 show that H1+ is more abundant than H2+ in the upper ionosphere. Therefore there is more of it for Saturn’s magnetosphere fields to pick up.
4.2 Ion densities
The results for the heaver species (HHC+, 70 amu and HNI+, 74 amu) are not shown here. Very little of these species are lost from the ionosphere. What does manage to escape leaves as very thin plasma streams that quickly break up into blobs of plasma. There is little difference between the density structures of these two species or the between structures in each of the cases.
4.3 The electric and magnetic fields
The main conclusion that can be made from the results presented above is that the orientation of the dayside ionosphere with respect to the incident flow to first order does not have an effect on the global features of Titan’s plasma interaction.
The ion loss rates are very close for each case. The radial flux of the ions passing through a spherical sampling region at 2500 km altitude show strong similarities in the location and magnitude of the ion fluxes. The reason for the similarities in the fluxes comes down to the configurations of the electric and magnetic fields. To first order the electric and magnetic fields around Titan are the same regardless of orientation of the dayside ionosphere. The resulting Poynting vector field has the same three-dimensional configuration as shown by the E × B streamlines in Figs. 27 and 28. The streamlines flow through the same regions in each case so the electromagnetic flux must go through the same regions. The ions respond to the electromagnetic flux and therefore the ion escape flux is nearly identical in all cases. The angle of illumination does not have a large effect on the ion loss from Titan.
There is a correlation between the relative amounts of each species being lost and the altitude of the ionospheric peak for that species. The higher the altitude of the ionospheric peak the larger the loss rate for that species. The main ion species lost by Titan are M+ and H1+. These correspond to the species represented by M+ in our model and represented by H1+. These species peak relatively high up in the ionosphere. The exception to the altitude trend is the loss of rate of the L+ species.
The L+ species peaks at the top of the ionosphere in the 1-dimensional photochemical model shown in Fig. 3. However, the peak ionization rate for this species occurs at an altitude of 1000 km (see Appendix A). The L+ created below 1500 km is chemically used to create M+ and H1+. Above 1500 km the reactions that create these species shut off and the L+ is allowed to build up in the photochemical model. The ionization rate is very small though less than 0.001 cm−3. Whatever L+ is created above 1500 km gets picked up by Saturn’s magnetosphere before it can build up and not much is being produced. The advection time scales and the chemical loss reaction rates are faster than the ionization rates for the L+ species.
The net loss rates reported here do not show a strong dependence on the orientation of the dayside ionosphere. Using Cassini observations Wahlund et al. (2005) report a net ion loss rate of 1 × 1025 s−1. Later estimates by Modolo et al. (2007) have upped the net loss rates to 2–7 × 1025 s−1. The net loss rate reported here is about half the rate of Wahlund et al. Part of this discrepancy may be due to the recent announcement that the initial INMS neutral densities reported were a factor of 3 too low (Waite, private communication). Increasing the neutral CH4 and N2 densities and the corresponding photo and secondary electron ionization rates will bring our ion loss rates into line with the results of Wahlund et al. and the lower limit reported by Modolo et al. There would be a 3 fold increase in the production of M+ and H1+ by ionization of the CH4 and N2. The increase in the M+ and H1+ densities will lead to an increase in the H2+, MHC+ and HNI+ via several chemical reactions. A further increase in the loss rate could occur if the electron impact ionization rates were increased. The electron impact rates used in this study are based on the CAPS electron fluxes measured during the TA encounter. The electron spectrum during this encounter is classified by Rymer et al. (2009) as a plasma sheet encounter. The peak electron energies in this region run between 120–600 eV with the fluxes at the peak energy between 3.5 × 105 and 1.2 × 106 cm−2 s−1 sr−1Rymer et al. (2009). Using electron production rates based on the higher end of these ranges would increase the nightside ionospheric densities and hence the ion loss from that region. There may be other factors that are not currently included in the present simulations that could contribute to ion loss from Titan. Neutral winds could help initially accelerate pickup ions leading potentially leading to a larger escape flux. Adding a realistic distribution of massive negative ions will change the currents in Titan’s ionosphere and could also potentially add to a larger escape flux. Of course further refinements to the ion-neutral chemistry model could also contribute.
The simulation results show that below 1200 km altitude densities in Titan’s ionosphere is in photochemical equilibrium. Above 1300 km altitude the densities are determined by the plasma advection. The plasma dynamics is of course determined by the electric and magnetic fields. The transition between chemical equilibrium and advection occurs somewhere between 1200–1300 km. This is in agreement with the range predicted by Ma et al. (2006).
Around Titan both the Hall and ∇ P e have significant effects on the electric and resulting magnetic fields. The Hall term is responsible for the large scale asymmetry about the flow axis in the orbital plane. It does not have an effect on the fields in the polar plane. Near Titan, the ∇ P e is a major contributor to the electric field. It is responsible for the twist and discontinuity in the electric field present upstream of Titan’s nose. It acts to decrease the electric field along the anti-Saturn hemisphere of Titan. The magnitude of the ∇ P e term is dependent on the electron density gradients in Titan’s ionosphere and the electron temperature. The electron density gradients in our model are determined by the chemistry and ion transport. The electron temperature is treated adiabatically above 1400 km altitude. Below 1400 km the temperature is set and held constant to match the Langmuir probe results reported by Ågren et al. (2009). This is reasonable since we do not include the electron-neutral cooling processes in the model. It is the region above our mask where the ∇ P e term is strongest.
To first order the electric and magnetic fields are in agreement between each of the cases. The higher order differences are due to ion pick up. The ion pick up, leads to blobs of plasma in the anti-Saturn facing flank. These plasma blobs feedback on the electric field creating waves and turbulence. This should be seen by Cassini out beyond 10RT from Titan when approaching from beyond Titan’s orbit. The turbulence does show a second order dependence on the location of the dayside ionosphere.
The main conclusions of this study, that the orientation of the dayside ionosphere has little effect on the ion loss rates from Titan is in agreement with the results of Sillanpää et al. (2006). There is a major topological difference between the present results and theirs. The ion tail in Sillanpää et al. was deflected by 45° with respect to the incident flow. This deflection was in the direction towards Saturn and into the convection electric field. The deflection is in the opposite direction indicated by the testparticle studies of Luhmann (1996), Ledvina et al. (2000, 2004b, 2005) and Tseng et al. (2008). Sillanpää et al. attribute this deflection to a conservation of momentum. As ions are picked up from Titan they move in the direction of the convection electric field, away from Saturn. The incident flow then is deflected in the opposite direction (towards Saturn) to conserve momentum. The deflection of the incident flow leads to the slow moving pickup ions being pulled along towards Saturn. The results presented here (see Fig. 13) do not show a deflection of the ion tail towards Saturn. The reason for the differences in the simulation results must be due to how the ionospheres are handled in the simulations. The ionosphere in Sillanpää et al. was treated has a perfectly conducting sphere that uniformly emitted plasma. Thus the ionosphere was a solid object. The ionosphere in this study was much softer. Fields were allowed to penetrate it due to collisional resistivity. The collisions also dampened the ion motion. The ionospheric density was a result of the driving equations responding to the incident conditions. Additionally the ∇ P e was shown to have a important effect on the electric fields around Titan. This resulted in an obstacle that is not spherically symmetric, not a uniform emitter of plasma and not a perfectly conducting sphere. As a result the large deflection of the ion tail towards Saturn reported by Sillanpää et al. is not present in the current simulation results.
The main conclusion to be remembered via these simulations is that to first order the orientation of the dayside ionosphere with respect to the incident flow does not affect the global scale features of Titan’s interaction with Saturn’s magnetosphere.
The ionosphere is in photochemical equilibrium below 1200 km. The transition between photochemical equilibrium and density profiles determined by advection occurs in a narrow shell 1200–1300 km altitude. The major ion species lost by Titan are represented by M+ and H1+, these correspond to and . There is a correlation between the ion loss rate of a given species and the altitude of its peak ionospheric density. The lower the altitude of the ionospheric density peak the lower the loss rate. These results are not strongly dependent on the orientation of the dayside ionosphere.
The electric field at the sub-flow point upstream of Titan contains a twist. This twist should correspond to a twist or kink in the magnetic field lines in this region. The twist is caused by a combination of the Hall and ∇ P e terms. The Hall term is responsible for the asymmetries in the fields seen in the orbital plane around Titan. While the ∇ P e term acts to decrease the electric field in the anti-Saturn facing flank.
Titan acts as a lens in the polar plane focusing the electromagnetic wave energy given by the Poynting field into the wake. While it acts as an astigmatic lens in the orbital plane. The wave energy is converged in the Saturn facing hemisphere and diverged in the anti-Saturn facing hemisphere. The slow moving plasma follow Poynting field as reflected in the density.
Titan’s interaction with Saturn’s magnetosphere is a complex and multifaceted problem. The research presented here shows that what was thought to be a major issue, the orientation of the dayside ionosphere, only has second order effects on the global scale of the interaction. Other parameter variations in the incident plasma or field parameters, as would be the case at different locations in Saturn’s magnetosphere should produce larger effects. While the second order effects are not important to the global interaction they may have a significant effect on the local evolution and energy balance of Titan’s ionosphere, atmosphere and the interaction between them. Localized heating of the atmosphere by ion precipitation may have a significant impact on the neutral density profiles. In addition it has been suggested that the neutral winds may have an influence on how the magnetic field slides around Titan (Cravens et al., 2010). These are just some of the outstanding issues that remain to be addressed.
The authors of this paper would like to acknowledge the support from NASA grant NNH09CE73C, and NASA grant NNX08AK95G. In addition, the authors would like to acknowledge the computational support provided by the NASA Advanced Supercomputer, NAS, scientific computing facility at NASA Ames Research Center Moffett field CA.
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