Measurements by the Cassini spacecraft during a close flyby of Saturn's moon Rhea on March 2, 2010, show the presence of intense plasma waves in the magnetic flux tube connected to the surface of the moon. Three types of waves were observed, (1) bursty electrostatic waves near the electron plasma frequency, (2) intense whistler-mode emissions below one half of the electron cyclotron frequency, and (3) broadband electrostatic waves at frequencies well below the ion plasma frequency. The waves near the electron plasma frequency are believed to be driven by a low energy (∼35 eV) electron beam accelerated away from Rhea. Their bursty structure is believed to be due to a nonlinear process similar to the three-wave interaction that occurs for Langmuir waves in the solar wind. The whistler-mode emissions are propagating toward Rhea and are shown to be generated by the loss-cone anisotropy (at parallel cyclotron resonance energies around 230 eV) caused by absorption of electrons at the surface of the moon. Scattering by these whistler-mode waves may be able to explain previously reported depletions of energetic electrons in the vicinity of the moon. The low-frequency waves may play a role in nonlinear three-wave interactions with the bursty electrostatic waves.
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 Saturn's largest icy moon Rhea orbits at a distance of 8.7 RS (Saturn's radii) from the center of the planet. Its internal geological activity is negligible [Pitman et al., 2008] and the passive interaction of the moon with Saturn's magnetosphere is believed to be the source of its tenuous oxygen–carbon dioxide atmosphere [Teolis et al., 2010]. Although Saturn's magnetosphere has only minor effects on the moon, Rhea strongly modifies the properties of the magnetospheric plasma in its vicinity [Wilson et al., 2010]. During the November 26, 2005 Cassini flyby of Rhea, a depletion of energetic electrons has been observed within several radii of the moon. Jones et al.  suggested that the depletion is caused by a disk of absorbing debris around Rhea, possibly in the form of discrete rings or arcs of material. This hypothesis is not consistent with direct optical observations which revealed no evidence of such material [Tiscareno et al., 2010]. No other explanation of the surprising depletions of electrons has been found so far. Interactions of the energetic electrons with various types of waves occurring in the magnetospheric plasma may play a role in the loss process causing these depletions. The purpose of this paper is to investigate the wave environment of Rhea in connection with properties of electron phase space density distributions and magnetic field. We discuss the generation mechanisms of the observed waves and their possible effects on energetic electrons.
2. Wave Environment of Rhea
 Measurements by the Cassini Radio and Plasma Wave instrument [Gurnett et al., 2004] during the March 2, 2010, close flyby of Rhea (Figure 1a) reveal that the moon generates a large variety of electrostatic and electromagnetic plasma waves (Figure 1d) that have important implications for the magnetospheric interactions occurring near the moon. Three types of plasma waves were observed; (1) Strong bursty emissions near the electron plasma frequency at 15–20 kHz; (2) Strong whistler-mode emissions below one half of the electron cyclotron frequency at 70 to 250 Hz; (3) Broadband electrostatic waves below about 40 Hz. These waves all occurred from about 1739 to 1742 UT, as the spacecraft passed through the magnetic flux tube connected to the surface of Rhea.
 The emissions around 15–20 kHz are at the same frequency as emissions near the electron plasma frequency in the surrounding magnetosphere of Saturn, but six orders of magnitude stronger. These waves are not accompanied by magnetic fluctuations and form wave packets (Figures 1b and 1c), similar to Langmuir waves in the Solar wind and foreshock regions [Gurnett et al., 1993]. The waves between 70 Hz and 250 Hz (∼0.1–0.4 of the electron cyclotron frequency) have a significant component of magnetic fluctuations (Figures 1e–1g) and are very similar to whistler-mode chorus emissions which are able to interact with energetic electrons [Horne et al., 2005], causing their diffusion in velocity space. The waves observed at frequencies below 40 Hz (below ∼0.1 of the proton plasma frequency) have no magnetic field component and are purely electrostatic (Figure 1h and 1i). Their amplitude abruptly decreases when the spacecraft moves away from the influence of the moon.
3. Plasma Environment of Rhea
 The observed electric and magnetic wave fields are clearly caused by plasma instabilities induced by Rhea. To understand the origin of the waves we have investigated the electron measurements obtained from the Cassini Plasma Spectrometer [Young et al., 2004]. Energy-time dynamic spectrograms of counts per accumulation from 4 selected anodes (out of 8) of the instrument in 63 logarithmic energy steps are shown in Figures 2a–2d. The accumulation time is 23.4 ms per energy step. The data reveal that the moon strongly modifies the electron velocity distributions. During the time interval for which we detect the fluctuating electromagnetic fields, we observe two distinct changes: (1) the electrons at energies above approximately 0.1–1 keV disappear in the direction coming from Rhea, presumably due to absorption by the moon, and (2) a dense electron beam coming from Rhea occurs at energies of 20–100 eV (G. H. Jones, et al., manuscript in preparation, 2011).
 We can note in Figures 1 and 2 that both the strong fluctuating electric and magnetic fields and the unstable features in the electron distributions occur and disappear at the same time. The time interval during which unstable features in the electron distributions occur corresponds to the passage of the spacecraft through the magnetic flux tube connected to the Rhea surface. Significant effects on electrons are not expected from the plasma corotation [Wilson et al., 2010], from the spacecraft orbital motion, from the orbital motion of Rhea, nor from the finite Larmor radius. The observed unstable features in the electron distributions between 20 eV and 10 keV should therefore map along the magnetic field lines with an accuracy better than 3% of the radius of Rhea. This mapping is confirmed by measurements of the Cassini fluxgate magnetometer [Dougherty et al., 2004] shown in Figure 3. The measurements also reveal that the magnetic field intensity is 10% stronger above the moon. This increase of the magnetic pressure is consistent with previous measurements in the Rhea wake [Jones et al., 2008; Khurana et al., 2008] which have been explained by a localized decrease of the plasma pressure. The same explanation can be used here for the observed effects in the flux tube above the absorbing body of the moon. Additionally, we observe a field-aligned current system related to Rhea. It can be roughly modeled by a homogeneous current density of −4 nA/m2 (directed from Rhea) inside the flux tube. The total integrated current from this model is 7.4 kA. At the boundary of the Rhea flux tube, the model doesn't accurately predict the measured magnetic field. As the variations are spiky, larger localized current densities reaching a few tens of nA/m2 can be expected here.
4. Bursty High-Frequency Electrostatic Waves
 Waves near the electron plasma frequency are known to be driven by electron beams [Gurnett and Bhattacharjee, 2005]. The electron beam at ∼35 eV shown in Figure 2f (its origin is analyzed by Jones et al. (manuscript in preparation, 2011)) is dense and cold enough to cause a positive slope in the reduced electron distribution function (Figure 2i),
We obtain ∂F/∂ v∥ ∼ 2 × 10−8 m−5s2 in the direction anti-parallel to the ambient magnetic field (Figure 2h) at a parallel velocity v∥ = v∥P ∼ −0.01c. This feature is unstable to the Landau resonance [Gurnett et al., 1993] and can generate waves in various modes, for example the Langmuir waves or obliquely propagating upper-hybrid waves. This is similar to the situation that produces type III radio emissions in the Solar wind [Reiner et al., 1995] where the instability in most cases causes a very rapid dissipation of the beam energy into unstable plasma waves, leading to observations of only marginally unstable ‘plateau’ distributions with ∂F/∂ v∥ ∼ 0. However, similar electron distributions with ∂F/∂ v∥ > 0 have been already observed in the solar wind, in connection with the type III radio bursts [Lin et al., 1986]. These distributions are consistent with our observations of very intense plasma fluctuations (see Figures 1b–1d). The Landau-unstable parallel wave numbers for v∥ = v∥P are
where f is the wave frequency. With f ∼ 18 kHz we obtain k∥P ∼ −3.8 × 10−2 m−1. The corresponding parallel wavelength is then L∥P ∼ 170 m, i.e., much larger than the Debye length of the core electron component (assuming a temperature of ∼20 eV we obtain λD ∼ 17m).
 Waves in Figure 1d show very broad-band frequency spectra. This spectral broadening could be hypothetically caused by the Doppler shift Δf resulting from the plasma corotation velocity vc = 57 km/s [Wilson et al., 2010] and a random perpendicular component of the wave vector k⊥,
For the observed Δf ∼ 5 kHz, we would, however, need unrealistically large values of k⊥ ∼ 0.6 m−1, for which the wavelengths would fall below the Debye length. A plausible explanation of the observed large bandwidth therefore is the presence of short-duration wave packets, documented in Figures 1b and 1c. They indicate the presence of local nonlinear microphysical processes; for example, three-wave interactions can link the low frequency ion acoustic waves, as those observed in Figure 1i, with bursty, impulsive plasma oscillations [Robinson et al., 1993] observed in Figures 1b–1d.
5. Whistler-Mode Waves
 Detailed wideband waveform measurements were made of the electric and magnetic fields at frequencies below 2.5 kHz where the whistler-mode waves occur. These waveforms are recorded in short snapshots of 2048 samples separated by long gaps of 48 s. One of these snapshots has been taken during 287 ms after 17:41:26.394 UT, in the final part of the Cassini passage through the Rhea magnetic flux tube. Figures 1e–1g show the waveforms measured by three orthogonal magnetic antennas. The BZ antenna is at a small angle from the background magnetic field B0, while the BX and BY antennas are nearly perpendicular to B0. The amplitudes of the measured BX and BY components reach 0.4–0.5 nT. This is approximately 2% of the strength ∣B0∣ which is 22.9 nT at the time of the waveform measurements. Compared to the amplitudes measured by the BZ antenna, the BX and BY amplitudes are approximately 3 times larger. This difference implies the presence of electromagnetic waves propagating with wave vectors at small angles from B0.
 Based on these measurements, we have performed a comprehensive polarization and propagation analysis of the observed waves. The three measured orthogonal components of the wave magnetic field have been transformed into a reference frame linked to the B0 direction. The analysis has been done in the frequency domain, where a broad peak of wave power is observed in Figure 4a at frequencies between 70 and 250 Hz which is between 0.1 and 0.4 of the electron cyclotron frequency (fce = 641 Hz at the time of the waveform measurements).
 We have used the singular value decomposition (SVD) method [Santolík et al., 2003] to analyze the magnetic-field polarization ellipsoid. The ratio of its two largest axes, plotted as Ellipticity in Figure 4g, is close to 1 which means a nearly circular polarization. The sign of this value is derived from the phase difference between the components along the two largest axes of the polarization ellipsoid, positive values mean right-handed polarization. These results show that the waves are propagating in the whistler mode. The smallest axis of the polarization ellipsoid is parallel to the wave vector. The angle θKB in Figure 4e shows that the waves propagate with wave vectors at angles less than 20° with respect to the B0 direction. The sign of the B0-component of the Poynting vector [Santolík et al., 2001] has been obtained from the three magnetic antennas and two electric antennas (Figure 4i). It shows positive values indicative of an energy flow from the Saturn's magnetosphere toward Rhea. Analysis of two other snapshots of multicomponent waveforms, recorded in the Rhea magnetic flux tube, shows whistler-mode waves with the same properties but with weaker intensities. Interestingly enough, one additional snapshot recorded after Cassini left the Rhea magnetic flux tube still shows intense whistler-mode waves with the same properties (Figure 4, right).
 The absorption of electrons by Rhea generates an unusually strong temperature anisotropy which is known to cause the first order cyclotron instabilities leading to emission of the whistler-mode waves. The v∥ - dependent anisotropy values can be obtained using the definition of Kennel and Petschek ,
Figure 2g shows that A (v∥) peaks at a value of ∼6 for v∥ = v∥A ∼ −0.03c. The region of A (v∥) > 1 extends to v∥ ∼ −0.1c. In other intervals of v∥ the anisotropy is close to zero. The parallel wave numbers unstable to the first order cyclotron resonance for v∥ = v∥A are
where fce is the electron cyclotron frequency.
 With fce = 630 Hz at the time of measurement of the electron phase space densities, and assuming f ∼ 0.3 fce (according to Figure 4a) we obtain an unstable parallel wave number of k∥A ∼ 3 × 10−4 m−1. This value exactly corresponds to the value obtained from the whistler-mode dispersion relation for this frequency. In other words, for the observed frequencies of the whistler mode waves, the parallel cyclotron resonance energy would be in the unstable region around 230 eV. An estimate of the linear growth rate of whistler-mode waves, according to Kennel and Petschek  is
With a roughly estimated plasma density of n ∼ 4 cm−3, based on the observations of the bursty plasma waves centered at a frequency of fp ∼ 18 kHz, with F(v∥A) ∼ 2 × 10−4 m−4s from Figure 2i, and with the fraction of resonant hot electrons η(v∥A) = v∥AF(v∥A)/n ∼ 4.5 × 10−4, we obtain a growth rate of γ/fce ∼ 4 × 10−3. Note that, unlike the Landau instability described in equation (2), the cyclotron instability in equation (5) generates, for the unstable features with v∥A < 0 (i.e., in the direction from Rhea) waves propagating with positive k∥ (i.e., from the Saturn's magnetosphere toward Rhea). The measurement of the sign of the parallel component of the Poynting flux in Figure 4i shows that the observed whistler-mode waves propagate toward Rhea. Note also, that the observed whistler-mode waves are the only electromagnetic waves observed in the Rhea flux tube. They can propagate large distances along the flux tube toward Rhea. Their group speed is directed approximately along the magnetic field line. The small but finite group velocity angles with respect to the magnetic field line cause these waves to be slightly spread outside the flux tube.
 Very high amplitudes of whistler-mode waves (more than 2% of the ambient magnetic field - see Figures 1f and 1g) would likely lead to nonlinear interactions with energetic electrons. Similar but relatively weaker emissions of whistler-mode chorus in the Earth's magnetosphere are known to cause pitch angle diffusion of energetic electrons [Ni et al., 2008] and their precipitation into the atmosphere [Nishimura et al., 2010], acting at similar spatial scales [Bortnik et al., 2008]. The empty slot region in the radiation belts is also attributed to whistler-mode waves [Bortnik et al., 2009]. We propose that strong whistler-mode waves which can propagate from large distances in the vicinity of the Rhea flux tube can act by a similar mechanism, effectively decreasing the flux of energetic electrons and thus possibly explaining the observed depletion of energetic electrons in the moon's vicinity [Jones et al., 2008]. A depletion of energetic electrons is indeed observed by Cassini also in this case (E. Roussos et al., manuscript in preparation, 2011).
 The observed large intensities of whistler-mode waves suggest that their amplitudes have been amplified by a factor of ∼105 from the background noise detected at these frequencies outside the Rhea flux tube. The whistler mode group speed at a frequency of 0.3 fce is approximately vG ∼ 6 × 106 m s−1 (i.e., vG ∼ 0.02 c). This, together with the above discussed growth rate, gives the characteristic e-folding scale of the linear convective growth of Le = vG/(2πγ) ∼ 380 km. The characteristic length necessary to amplify the waves to the observed amplitudes is then very short compared to the scale of the Saturn's magnetosphere, L = Le ln (105) ∼ 4400 km. This length, however, is probably unrealistically short and a larger amplification region would be necessary in reality. The unstable features of the observed phase space density (its large anisotropy) are likely to be the strongest at the point of observation close to Rhea and they will weaken with the distance from the moon. The growth rates will be therefore lower further out from Rhea and the waves may need somewhat larger lengths to be amplified to the observed amplitudes.
 Understanding generation and effects of these intense plasma waves is important not just to Rhea, and not just to Saturn but to all planetary magnetospheres. This also includes the Earth's magnetosphere, where intense whistler-mode chorus waves have been shown to contribute to both loss and acceleration [Bortnik et al., 2008, 2009] of relativistic electrons in the outer Van Allen radiation belt.
 Cassini-Huygens is a mission of international collaboration between NASA, the European Space Agency (ESA), and the Agenzia Spaziale Italiana (ASI). The research at the University of Iowa was supported by NASA through contract 1415150 with the Jet Propulsion Laboratory. O.S. acknowledges additional support from grants CACR P205-10-2279, ME10001, and LH11122. G.H.J. is supported by a UK STFC Advanced Fellowship. Cassini work at MSSL-UCL is supported by STFC, the UK Space Agency, and ESA.
 The Editor thanks one anonymous reviewer for his//her assistance in evaluating this paper.