- Open Access
Ion acceleration by multiple reflections at Martian bow shock
© 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: 4 February 2011
- Accepted: 12 July 2011
- Published: 8 March 2012
The ion mass analyzer (IMA) on board Mars Express revealed bundled structures of ions in the energy domain within a distance of a proton gyroradius from the Martian bow shock. Seven prominent traversals during 2005 were examined when the energy-bunched structure was observed together with pick-up ions of exospheric origin, the latter of which is used to determine the local magnetic field orientation from its circular trajectory in velocity space. These seven traversals include different bow shock configurations: (a) quasi-perpendicular shock with its specular direction of the solar wind more perpendicular to the magnetic field (QT), (b) quasi-perpendicular shock with its specular reflection direction of the solar wind more along the magnetic field (FS), and (c) quasi-parallel (QL) shock. In all seven cases, the velocity components of the energy-bunched structure are consistent with multiple specular reflections of the solar wind at the bow shock up to at least two reflections. The accelerated solar wind ions after two specular reflections have large parallel components with respect to the magnetic field for both QL cases whereas the field-aligned speed is much smaller than the perpendicular speed for all QT cases.
- bow shock
Collisionless shocks such as interplanetary shocks (Gloeckler et al., 1994) and bow shocks of planets, e.g., Earth (Paschmann et al., 1981; Sckopke et al., 1983, 1990) and Mars (Afonin et al., 1989; McKenna-Lawlor et al., 1998; Dubinin et al., 2006; Yamauchi et al., 2011) are known to accelerate ions. The accelerated ions at the terrestrial bow shock are observed as both diffuse distributions and discrete distributions in the energy domain (Bale et al., 2005; Burgess et al., 2005; Eastwood et al., 2005). An example of the diffuse distribution is the foreshock diffuse component (Gosling et al., 1978), and it has been explained mainly by Fermi acceleration. Examples of the discrete distribution are field-aligned beams and reflected gyrating ions (Gosling et al., 1978, 1982; Sckopke et al., 1983, 1990), and they have been explained by reflection at the bow shock (e.g., Burgess and Schwartz, 1984; Oka et al., 2005) and wave-particle interactions (e.g., Meziane et al., 2001; Mazelle et al., 2003), although the exact mechanisms are open questions. One consequence of reflection modeling is that some ions may go through multiple reflections or surfing (Sagdeev, 1966) to reach high energies. This model is further developed for thin shock case (Lee et al., 1996; Zank et al., 1996). The multiple reflections can also be the precondition for escape from the bow shock to form the foreshock (e.g., Oka et al., 2005), although multiple reflections have not been observed for the terrestrial bow shock.
Figure 1(a) shows energy-time spectrograms of electron energy flux and proton energy flux observed by the ELectron Spectrometer (ELS) and IMA, respectively, during an outbound traversal from the frank bow shock to the upstream region on 12 July, 2005. The bow shock crossing is at around 11:34:30 UT. Solar wind protons are seen at around 0.7 keV (He++ contamination is seen at around 1.4 keV) every 192 sec that corresponds to a scanning cycle of the field-of-view of IMA. Above the solar wind energy, energy-bunched stripes are observed at around 2 keV, 3 keV, and 5 keV. The lowest-energy branch is pick-up ions of exospheric origin (Dubinin et al., 2006; Yamauchi et al., 2006). Figure 1(b) shows ion data for azimuthal directions (22.5° wide each) that registered these energy-bunched stripes during one of 192-sec cycles of the ion observation. The energy-bunched stripes at energies higher than that of the pick-up ions are marked by orange (around 3 keV) and red (around 5 keV). Signatures of the other possible branches (around 6∼8 keV) are also marked using different colors. Figure 1(c) shows the velocity scatter plot of protons for the same data using the same colors as Fig. 1(b), projected into planes along and perpendicular with respect to the estimated magnetic field direction (−N), respectively.
In Yamauchi et al. (2011), the same calculation was made for the second reflection because these reflected solar wind ions are expected to return back to the bow shock. If the bow shock is laminar, the incident angle of these returning ions to the bow shock will be very narrow, and hence the reflection can again be collimated to a narrow direction. The expected jump and trajectory are given by red arrow, red dashed circle, and red horizontal line, similar to the first reflection (orange color). They are consistent with the third ring distribution (red cross and pink triangle) which is col-limated to a small velocity space. Such a collimation cannot be achieved by pick-up ions because they have wide phase angles for injection when they are reflected at the bow shock. Also, the intensity of the third ring cannot be explained by the reflection of the pick up ions. Therefore, Yamauchi et al. (2011) concluded that two main branches at energies higher than that of the pick-up ions represent a single and double specular reflections of solar wind protons at the bow shock, respectively. The specular reflection model agrees only in the Mars frame and not in the solar wind frame or de Hoffman-Teller frame that are sometimes used (e.g., Burgess and Schwartz, 1984).
As the possible cause for the multiple reflection specific to Mars but not reported at the Earth or Venus, Yamauchi et al. (2011) considered possible factors that makes Mars qualitatively different from Venus or Earth, namely the finite gyroradius effect compared to the radius of the bow shock curvature and the abundance of residual cold ions of exospheric origin near the Martian bow shock (Dubinin et al., 1993). They demonstrated that the finite gyroradius effect makes the reflected ion easier to escape, i.e., more difficult to return back to the bow shock, whereas the cold ions near the Martian bow shock forms a third plasma population (others are the solar wind and the magnetosheath ions), making it possible to have a new “characteristic speed” which enables the double-foot structure as observed, and making the returning of the reflected ions easier. If this is true, we expect the multiple reflections at the Martian bow shock occur very often. So far, Yamauchi et al. (2011) showed only one example of quantitative examination due to the difficulty in deriving the magnetic field orientation. One example is not enough to draw a general conclusion. Furthermore, bow shock accelerations are different between quasi-perpendicular shocks and quasi-parallel shocks (e.g., Bale et al., 2005; Burgess et al., 2005). Therefore, more case studies with the same quantitative level are needed.
This type of analysis normally requires a statistical study; however, the Martian data existing to date are not suitable for statistical study because MEX does not carry a magnetometer for obtaining pitch-angles of observed ions even though MEX is the only spacecraft that produced a sufficient quantity of ion data at the relevant energies near the Martian bow shock for a statistical study. Although the local magnetic field orientation can sometimes be estimated from pick-up ions of exospheric origin, this method is not suitable for statistical studies when other ions (accelerated ions in the present case) overlay the pick-up ions (Yamauchi et al., 2011). In this paper, we examined the best cases from one-year of data (during 2005), i.e., when the energy-bunched structure is observed together with pick-up ions from the newly ionized hydrogen corona with a good separation in velocity space.
Here, we subdivide the observations into three categories in terms of shock types and the expected pitch angle of the specularly reflected solar wind in the Mars frame as illustrated in Fig. 3: (a) quasi-perpendicular shock by which specular reflection direction is nearly perpendicular to the magnetic field; (b) quasi-perpendicular shock by which specular reflection direction is oblique or parallel to the magnetic field (foreshock configuration); and (c) quasi-parallel shock. We hereafter abbreviate these three types as QT, FS, and QL, respectively. A point that belongs to the FS bow shock is normally 90° away in the azimuthal (Y-Z) direction from a point that belongs to the QT shock as illustrated in Fig. 3(d). The difference between the FS and the QT cases is important in considering the pitch angle of specularly reflected solar wind because one must consider observation in the Mar frame and not in the de Hoffman-Teller frame. The difference in the reference frames is important in the flank region where angle between the bow shock normal and the sun direction is more than 45°.
Note that it is nearly impossible to find an ideal quasi-parallel case with MEX that does not carry the magnetometer (Yamauchi et al., 2008). For all examined traversals, IMA’s ion counts at energies more than 0.5 keV that are observed outside the bow shock are manually classified into ions from the solar wind, pickup ions with zero initial velocity (“primary ring distribution” in ion spectrograms), and accelerated ions. Electron data (ELS) is also used to supplement the ion data for identifying the shock crossings.
IMA and ELS are parts of the Analyzer of Space Plasma and Energetic Atoms (ASPERA-3) experiment on board MEX. IMA is a top hat instrument that combines an electrostatic energy analyzer with a magnetic mass analyzer. IMA measures ions in the energy range from 10 eV/q to 30 keV/q in 96 logarithmically scaled energy steps every 12 sec. IMA has a 4.6° × 360° field of view, where the 360° measurement plane is divided into 16 azimuthal sectors (0–15), each 22.5° wide. Out of 16 sectors, ϕ = 0 is strongly contaminated from the other sectors, and we do not use it for the present analyses. IMA has an extra electrostatic deflection system (or elevation analyzer) at its entrance, which scans from −45° to +45° (16 elevations) in 192 sec. Therefore, IMA energy-time spectrograms have a 192-sec cycle, within which the spectrogram is seen as an energy-polar angle spectrogram. The overall field-of-view is approximately 360° (16 sectors = ϕ) × 90° (16 elevations = θ). ELS is a top hat instrument that measures electrons, and has a 4° × 360° field of view, which is divided into 16 azimuthal sectors, each 22.5° wide. ELS covers an energy range from 1 eV to 20 keV. In 2005, ELS measured from a plane which was parallel to the IMA 0° elevation plane. For details of the IMA and ELS instruments, see Barabash et al. (2006), Fedorov et al. (2006), and Frahm et al. (2006).
The orientation of the interplanetary magnetic field (IMF) is estimated from the ring distribution of newly-born ions coming from the planetary exosphere using the same method as that described in Yamauchi et al. (2011): These primary ring distribution is used to obtain the local L-M-N right-handed Cartesian coordinates through the minimum variance method, where N is the estimated IMF orientation (Yamauchi et al., 2006). In addition, L X = 0 is imposed to fill the last degree of freedom in the minimum variance method (this method constrains five components out of the total six components of L and M), and the average V N is assumed to be zero for the primary ring ions (Yamauchi et al., 2011). This method is useful only when the IMF orientation is optimum because of the restrictive field of view of IMA due to the restrictive MEX attitude (driven by the camera which always faces the nadir direction).
Selected seven traversals.
29 July 2005
3 Aug. 2005
5 Aug. 2005
22 Nov. 2005
29 Nov. 2005
3 June 2005
12 July 2005
Figure 4 shows the overview of proton and electron data from the first five traversals (#1 to #5) in the same format as Fig. 1(a). The electron data show fairly steady solar wind conditions, with increasing average energy toward the bow shock at very close distance. The ion data shows several discrete bands at higher energy from that of the solar wind protons. These discrete bands do not correlate with any features in the electron data except during the bow shock crossing. Ions with the lowest band in energy and with the longest stretch in the elevation direction (the primary ring distribution) represent pick-up ions of exospheric hydrogen (Yamauchi et al., 2006, 2011), from which the orientation of the local magnetic field is estimated.
Using the same procedure as Yamauchi et al. (2011), the local L-M-N coordinate system was obtained for each full scan (192 sec), and the velocity space points that registered five counts or more during the 100 ms measurement period are drawn in the V L -V N projection (upper panels) and V L -V M projection (lower panels) for eight selected full scans from these many scans (other 192-sec scans are similar or less prominent) in Fig. 5 in the same format as Fig. 1(c). The corresponding energy versus elevation/time spectrograms that have been divided into different azimuthal sectors are shown in Fig. 6 (same format as Fig. 1(b)) such that one can relate the classification to the raw data.
We need both Figs. 5 and 6 in the analyses because IMA does not cover all 4p direction and some of its field-of-view is blocked by the spacecraft (Yamauchi et al., 2011). The non-visible direction lies mostly at the lower part of the V L -V M plots. Different energy-bunched stripes in Fig. 6 are classified using different colors in the similar way as Yamauchi et al. (2011), and these colors are used in Fig. 5: solar wind by light blue, the primary ring distribution by blue, the second ring distribution at energy higher than the primary ring distribution by orange, the third ring distribution at energy higher than the second ring distribution by red, and the other major clusters of counts by purple and green. The pink color is used for possible extension but disconnected from the red-colored branch.
Selected seven traversals.
N in MSO
n in LMN
V R1 /VSW in LMN
(−0.05, +0.94, +0.34)
(+0.62, −0.74, −0.26)
(+0.93, −0.12, −0.35)
(+0.05, +0.95, −0.25)
(+0.68, −0.73, −0.07)
(+0.99, −0.08, +0.07)
(+0.74, −0.18, +0.65)
(−0.07, +0.79, +0.61)
(+0.32, −0.59, −0.74)
(+0.42, +0.24, −0.88)
(+0.62, +0.05, +0.78)
(−0.52, −0.82, −0.26)
(−0.88, −0.45, −0.15)
(+0.62, −0.07, +0.79)
(+0.57, −0.56, +0.60)
(−0.53, −0.29, +0.80)
(−0.28, −0.74, −0.61)
Selected seven traversals.
V I2 /VSW
V R2 /V SW
(+0.8, +2.2, −0.4)
(+2.1, +0.7, −0.9)
(−0.4, +1.4, +0.8)
(0, 1.0, -1.2)
By studying the 12 July 2005 event, Yamauchi et al. (2011) concluded that the second ring distribution is specularly reflected solar wind at the bow shock (cf. Fig. 1(c)). To examine this for the present examples, we calculated the velocities of reflected solar wind from the bow shocks with normal direction n by assuming a specular reflection given by Eq. (1). The seventh and eighth columns in Table 2 show the estimated velocity and its error range (normalized by the solar wind speed) after the reflection in the L-M-N coordinates, respectively. The error range is calculated by assuming ±5° of uncertainty in the direction of n in both X and Y directions (the same as Yamauchi et al. (2011)). The calculated reflections are drawn using orange arrows in Fig. 5. The start and end of each arrow correspond to injection (solar wind) and reflection velocities, respectively. Due to the gyromotion of ions around the local magnetic field (V N axis) in the solar wind frame, a reflected solar wind ion follows a circular trajectory in the V L -V M plane as drawn using orange dashed circle while keeping a constant V N that is given by orange horizontal lines in Fig. 5 (the same as Fig. 1(c)). The observed secondary ring distribution (orange empty triangles) is found near such predicted trajectories.
Yamauchi et al. (2011) further showed that the third ring distribution at energy higher than the second ring distribution in the 12 July 2005 event agrees with second reflection of the reflected solar wind ions at the bow shock, as shown in Fig. 1(c). In this example, the clustered ions are found only within a short extension in the elevation direction, making a gyrophase bunched distribution as one can see in Figs. 1(a) and 1(b). The velocity that corresponds to the disappearance of the secondary ring distribution has a large anti-sunward speed (larger than the solar wind speed) and flowing toward the bow shock with normal n as one can see in Fig. 1(c). Therefore, the gyrophase that corresponds to the second injection to the bow shock (first injection is the solar wind) was assumed to be about the same as where the cluster of secondary ring distribution disappears.
The same type of gyrophase bunching and the large anti-sunward speed at the end of this bunching are observed in all cases in Figs. 4–6. Therefore, we assume the same, i.e., that the observed gyrophase extent (disappearance) of the second ring corresponds to the lost due to the second reflection. The velocities of the assumed second injection normalized by the solar wind speed in the L-M-N coordinates are shown in the fourth column of Table 3. The corresponding gyrophase angles in the solar wind frame are also shown in the fifth column. Since the ring distribution is aligned to the elevation direction (angular resolution is less than 10°) as shown in Fig. 4, the error range of the terminating gyrophase is about ±10°, while we assumed the same shock normal n between the first and second reflections because most of the observations are where the bow shock curvature is small compared to the reflected solar wind. This procedure automatically assumes the direction of the gyration, which indicates the sign of the magnetic field polarity (sign of the fifth column in Table 3, where plus means clockwise rotation and minus means counter-clockwise rotation in Fig. 5).
Using these injection velocities, velocities of second specular reflections are calculated. The velocity and their error range in the L-M-N coordinates (normalized by the solar wind speed) are summarized in the sixth and seventh columns of Table 3. A secondary reflected ion again performs gyromotion around the IMF (V N axis) in the solar wind frame, and it follows a circular trajectory in the V L -V M plane while keeping a constant V N . The jump of the velocity by this reflection in the V L -V M projection is also drawn by red arrows in Fig. 5, and the following gyromotion is drawn by a red dashed circle. The same prediction is also made in the field-aligned direction, as given by the red horizontal lines in the V L -V N projection. The observed third ring (red cross) in Fig. 5 is found at velocity space near this prediction for all cases, and therefore, the third ring distribution is well explained by the secondary specular reflection of the solar wind ions.
Note that possible extensions of the third ring that are marked by pink colors for 5 Aug 2005 event (#3a) and 3 June 2005 events (#6a, #6b) are slightly off from the expected gyrating trajectory. This means that the pink-marked ions and red-marked ions are not on the same trajectory in velocity space. Since the bow shock normal direction is not constant in both time and space, such a fluctuation is quite possible, constructing a deformed ring trajectory. In fact, the magnetic field direction changed dynamically during the traversal of 3 June, 2005 (Yamauchi et al., 2008).
Figure 5 shows another clustered population marked by green triangles. This population extends from velocity space point that is very close to the primary ring distribution, whereas it does not resemble to the foot ions that are studied in Yamauchi et al. (2011). We have no solid interpretation for this population, and can only speculate that it might be related to the interaction between the pick-up ions and the bow shock. Note that pick-up ions can enter the bow shock at wide gyro-phases, and cannot introduce the narrow reflection direction that is necessary for energy-bunched second and third rings.
We have examined seven different examples of which six are the best traversals during 2005 of multiple energy-bunched protons at energies higher than the pickup ions of exospheric origin (zero-velocity in the planetary rest frame). In all cases that are summarized in Tables 1 and 2, the second branch marked by orange colors in Figs. 5 and 6 are consistent with specular reflections of the solar wind at the bow shock in the Mars frame (Sagdeev, 1966; Gosling et al., 1978; Paschmann et al., 1980, 1981; Dubinin et al., 2006; Yamauchi et al., 2011); i.e., both parallel velocity and perpendicular speed in the solar wind frame (with respect to the magnetic field) of the specularly reflected solar wind agrees with those of the energy-bunched ions marked by the orange color. A large part of the data is further consistent with second reflection of these orange-marked ions, although some traversals have ion populations that do not belong to this explanation.
We also examined two observations from the 3 June 2005 traversal when the IMF changed quickly. The first observation at around 06:07 UT (#6a) showed energy-bunching that is consistent with the multiple specular reflections at the bow shock. The other observation at around 06:13 UT (#6b) showed weak ion counts that is consistent with the multiple reflection and a substantial counts of accelerated ions that does not agree with the reflection prediction. However, the latter is somewhat similar to #6a with less intensity, and might be remaining from the old population because a temporal variation in the IMF can easily cause a reconfiguration of the bow shock or even non-planer bow shock. The energized ions arriving at the IMA instrument during 06:11:24∼06:14:36 UT might have come from a different region than the pick-up ions.
Except #6b mentioned above, the predicted reflection direction with respect to the estimated magnetic field orientation agrees with the observed energy-bunched stripes, and this direction is summarized in the eighth column in Table 3 (observation is shown for #6b). Perpendicular accelerations (#1a, #2a, #5a, #6a) are consistently seen in the QT shocks, whereas parallel accelerations (#3a, #6b, #7a) are seen in the QL and FS shocks. In this sense, the sub-classification of the quasi-perpendicular shock into QT and FS turned out to be useful. The other cases (#2b, #4a) are marginal and consistent with the above relation. These relations agree with the terrestrial bow shock where foreshock ions are found upstream of the quasi-parallel shocks (e.g., Eastwood et al., 2005; and references therein).
The ninth and tenth columns of Table 3 summarize VdHT and its error range in the field-aligned direction by assuming ±5° uncertainty in the direction of n. Except for 3 June 2005 events (#6a, #6b) and 5 August 2005 event (#3a), ǀVdHTǀ/VSW >1.5. Furthermore, the error in the field-aligned component of VdHT is larger than half the solar wind speed in 5 examples. Therefore, our estimate of the escape condition in the presented examples has large uncertainty.
On the other hand, all events with parallel acceleration (#3a, #6b, #7a) correspond to escape beyond the uncertainty after the second reflection, as summarized in eleventh column of Table 3. The velocities after the first reflection in these events are marginal (between escape and being trapped), and the finite gyroradius of ions cause them to hit the bow shock again (Yamauchi et al., 2011). The events with perpendicular acceleration correspond to trapping, although the uncertainty is large for these cases. From these results, escape from the bow shock seems to require a configuration in which ions are reflected toward the field-aligned direction such as at the QL shocks.
In the present study, we have examined only cases when multiple accelerations (energy-bunched structures) are observed. We did not examine general cases when such structure is not observed such as the case of 3 June 2005 (#6a, #6b). The latter study is needed to know the probability of observing the energy-bunched structures. Unfortunately, such a statistical study is difficult, if not impossible, without a magnetometer. We leave it to the future studies from a new Martian mission with a full plasma-field package.
In all examples that are ideal for analyses during 2005, the intense counts at higher energy than the primary ring distribution are often found immediately outside the Martian bow shock, and these intense counts at energies of several to tens keV are most likely accelerated solar wind ions by multiple specular reflections at the bow shock. Although the present study is not statistically strong, the data support common occurrence of multiple specular reflection of the solar wind at the bow shock, and hence support the explanation by the abundance of cold ions at the Martian bow shock as the reason for the speciality of Mars, i.e., not reported at the Earth or Venus (Yamauchi et al., 2011).
Let us consider the possible consequence if the cold ambient ions caused the solar wind acceleration by multiple reflections at the bow shock. Combination of the cold ions and the shocks is expected in the interstellar medium because it is rich in cold neutrals. For example, shocks associated with supernova explosions may have abundant cold ions. Since the multiple reflection mechanism is very effective for bulk acceleration, it may well pre-accelerate ions at the supernova remnant shock before the Fermi acceleration takes over to create galactic cosmic rays. A similar mechanism has been simulated for electrons (Amano and Hoshino, 2009), and we need similar simulation for ions in the future.
This work was partly supported by the Swedish Research Counsel (VR) #621-2008-3769 and Swedish National Space Board (RS) in Sweden, and by NASA contract NASW-00003 at SwRI, in the USA. The lead author (MY) wishes to thank Sweden programs of providing help for physically disabled individuals which have made it possible for him to conduct this work.
Guest editor J. S. Halekas thanks two anonymous reviewers for their assistance in evaluating this paper.
- Afonin, V., S. McKenna-Lawlor, K. Gringauz, K. Kecskemety, E. Keppler, E. Kirsch, A. Richter, D. O’Sullivan, A. Somogyi, A. Thompson, A. Varga, and M. Witte, Energetic ions in the close environment of Mars and particle shadowing by the planet, Nature, 341, 616–618, doi:10.1038/341616a0, 1989.View ArticleGoogle Scholar
- Amano, T. and M. Hoshino, Electron shock surfing acceleration in multidimensions: Two-dimensional particle-in-cell simulation of collisionless perpendicular shock, Astrophys. J., 690, 244–251, doi:10.1088/0004-637X/690/1/244, 2009.View ArticleGoogle Scholar
- Bale, S. D., M. A. Balikhin, T. S. Horbury, V. V. Krasnoselskikh, H. Kucharek, E. Möbius, S. N. Walker et al., Quasi-perpendicular shock structure and processes, Space Sci. Rev., 118, 161–203, doi:10.1007/s11214-005-3827-0, 2005.View ArticleGoogle Scholar
- Barabash, S., R. Lundin, H. Andersson, K. Brinkfeldt, A. Grigoriev, H. Gunell et al., The analyzer of space plasmas and energetic atoms (ASPERA-3) for the Mars Express mission, Space Sci. Rev., 126(1–4), 113–164, doi:10.1007/s11214-006-9124-8, 2006.Google Scholar
- Burgess, D. and S. J. Schwartz, The Dynamics and upstream distributions of ions reflected at the Earth’s bow shock, J. Geophys. Res., 89(A9), 7407–7422, doi:10.1029/JA089iA09p0740, 1984.View ArticleGoogle Scholar
- Burgess, D., E. A. Lucek, M. Scholer, S. D. Bale, M. A. Balikhin, A. Balogh, T. S. Horbury, V. V. Krasnoselskikh, H. Kucharek, B. Lembege, E. Möbius, S. J. Schwartz, M. F. Thomsen, and S. N. Walker, Quasi-parallel shock structure and processes, Space Sci. Rev., 118, 205–222, doi:10.1007/s11214-005-3827-0, 2005.View ArticleGoogle Scholar
- Dubinin, E., R. Lundin, H. Koskinen, and O. Norberg, Cold ions at the Martian bow shock phobos observations, J. Geophys. Res., 98, 5617–5623,1993.View ArticleGoogle Scholar
- Dubinin, E., M. Fraenz, J. Woch, S. Barabash, R. Lundin, and M. Yamauchi, Hydrogen exosphere at Mars: Pickup protons and their acceleration at the bow shock, Geophys. Res. Lett., 33, L22103, doi:10.1029/2006GL027799, 2006.View ArticleGoogle Scholar
- Eastwood, J. P., E. A. Lucek, C. Mazelle, K. Meziane, Y. Narita, J. Pickett, and R. A. Treumann, The foreshock, Space Sci. Rev., 118, 41–94, doi:10.1007/s11214-005-3824-3, 2005.View ArticleGoogle Scholar
- Fedorov, A., E. Budnik, J.-A. Sauvaud, C. Mazelle, S. Barabash, R. Lundin et al., Structure of the Martian wake, Icarus, 182(2), 329–336, doi:10.1016/j.icarus.2005.09.021, 2006.View ArticleGoogle Scholar
- Frahm, R. A., J. D. Winningham, J. R. Sharber, J. R. Scherrer, S. J. Jeffers, A. J. Coates, D. R. Linder, D. O. Kataria, R. Lundin, and S. Barabash et al., Carbon dioxide photoelectron energy peaks at Mars, Icarus, 182, 371–382, 2006.View ArticleGoogle Scholar
- Gloeckler, G., J. Geiss, E. C. Roelof, L. A. Fisk, F M. Ipavich, K. W. Ogilvie, L. J. Lanzerotti, R. von Steiger, and B. Wilken, Acceleration of Interstellar Pickup Ions in the Disturbed Solar Wind Observed on Ulysses,J. Geophys.Res., 99(A9), 17637–17643, 1994.View ArticleGoogle Scholar
- Gosling, J. T., J. R. Asbridge, S. J. Bame, G. Paschmann, and N. Sckopke, Observations of two distinct populations of bow shock ions in the upstream solar wind, Geophys. Res. Lett., 5(11), 957–960, 1978.View ArticleGoogle Scholar
- Gosling, J. T., M. F. Thomsen, S. J. Bame, W C. Feldman, G. Paschmann, and N. Sckopke, Evidence for specularly reflected ions upstream from the quasi-parallel bow shock, Geophys. Res. Lett., 9(12), 1333–1336, 1982.View ArticleGoogle Scholar
- Lee, M. A., V. D. Shapiro, and R. Z. Sagdeev, Pickup ion energization by shock surfing, J. Geophys. Res., 101(A3), 4777–4789, 1996.View ArticleGoogle Scholar
- Mazelle, C, K. Meziane, D. Le Queau, M. Wilber, J. P. Eastwood, H. Re, J. A. Sauvaud et al., Production of gyrating ions from nonlinear wave-particle interaction upstream from the Earth’s bow shock: a case study from Cluster-CIS, Planet. Space Sci., 51, 785–795, 2003.View ArticleGoogle Scholar
- McKenna-Lawlor, S., V. V. Afonin, E. Kirsch, K. Schwingenschuh, J. A. Slavin, and J. G. Trotignon, An overview of energetic particles (from 55keV to > 30 MeV) recorded in the close Martian environment, and their energization in local and external processes, Planet. Space Sci., 46, 83–102, 1998.View ArticleGoogle Scholar
- Meziane, K., C. Mazelle, R. P. Lin, D. LeQuéau, D. E. Larson, G. K. Parks, and R. P. Lepping, Three-dimensional observations of gyrating ion distributions far upstream from the Earth’s bow shock and their association with low-frequency waves, J. Geophys. Res., 106, 5731–5742, 2001.View ArticleGoogle Scholar
- Oka, M., T. Terasawa, Y Saito, and T. Mukai, Field-aligned beam observations at the quasi-perpendicular bow shock: Generation and shock angle dependence, J. Geophys. Res., 110, A05101, doi:10.1029/2004JA010688, 2005.Google Scholar
- Paschmann, G., N. Sckopke, J. R. Asbridge, S. J. Bame, and J. T. Gosling, Energization of solar wind ions by reflection from the Earth’s bow shock, J. Geophys. Res., 85, 4689–4693, 1980.View ArticleGoogle Scholar
- Paschmann, G., N. Sckopke, I. Papamastorakis, J. R. Asbridge, S. J. Bame, and J. T. Gosling, Characteristics of reflected and diffuse ions upstream from the Earth’s bow shock, J. Geophys. Res., 86, 4355–4364, 1981.View ArticleGoogle Scholar
- Sagdeev, R. Z., Cooperative phenomena and shock waves in collisionless plasmas, in Reviews of Plasma Physics, vol. 4, edited by M. A. Leontovich, p. 23, Consultants Bur., New York, 1966.Google Scholar
- Sckopke, N., G. Paschmann, S. J. Bame, J. T. Gosling, and C. T. Russell, Evolution of ion distributions across the nearly perpendicular bow shock: Specularly and non-specularly reflected-gyrating ions, J. Geophys. Res., 88, 6121–6136, 1983.View ArticleGoogle Scholar
- Sckopke, N., G. Paschmann, A. L. Brinca, C. W. Carlson, and H. Luhr, Ion thermalization in quasi-perpendicular shocks involving reflected ions, J. Geophys. Res., 95, 6337–6352, 1990.View ArticleGoogle Scholar
- Vignes, D., C. Mazelle, H. Reme, M. H. Acuna, J. E. P. Connerney, R. P. Lin, D. L. Mitchell, P. Cloutier, D. H. Crider, and N. F. Ness, The solar wind interaction with Mars: Locations and shapes of the bow shock and the magnetic pile-up boundary from the observations of the MAG/ER Experiment onboard Mars Global Surveyor, Geophys. Res. Lett., 27(1), 49–52, doi:10.1029/1999GL010703, 2000.View ArticleGoogle Scholar
- Yamauchi, M., Y. Futaana, A. Fedorov, E. Dubinin, R. Lundin, J.-A. Sauvaud, D. Winningham, R. Frahm, S. Barabash et al., IMF direction derivation from cycloid-like ion distributions observed by Mars Express, Space Sci. Rev., 126(1–4), 239–266, doi:10.1007/s11214-006-9090-1, 2006.Google Scholar
- Yamauchi, M., Y. Futaana, A. Fedorov, E. Kallio, R. A. Frahm, R. Lundin, J.-A. Sauvaud, D. J. Winningham, S. Barabash, and M. Holmström, Advanced method to derive the IMF direction near Mars from cycloidal proton distributions, Planet. Space Sci., 56(8), 1145–1154, doi:10.1016/j.pss.2008.02.012, 2008.View ArticleGoogle Scholar
- Yamauchi, M., Y. Futaana, E. Fedorov, R. A. Frahm, J. D. Winningham, E. Dubinin, R. Lundin, S. Barabash, M. Holmström, C. Mazelle, J.-A. Sauvaud, T. L. Zhang, W. Baumjohann, A. J. Coates, and M. Fraenz, Comparison of accelerated ion populations observed upstream of the bow shocks at Venus and Mars, Ann. Geophys., 29, 511–528, doi:10.5194/angeo-29-511-2011, 2011.View ArticleGoogle Scholar
- Zank, G. P., H. L. Pauls, I. H. Cairns, and G. M. Webb, Interstellar pickup ions and quasi-perpendicular shocks: Implications for the termination shock and interplanetary shocks, J. Geophys. Res., 10 1(A1), 457–477, 1996.View ArticleGoogle Scholar