2016
DOI: 10.1016/j.icarus.2016.01.032
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Characteristics of proton velocity distribution functions in the near-lunar wake from Chandrayaan-1/SWIM observations

Abstract: Due to the high absorption of solar wind plasma on the lunar dayside, a large scale wake structure is formed downstream of the Moon. However, recent in-situ observations have revealed the presence of protons in the near-lunar wake (100 km to 200 km from the surface). The solar wind, either directly or after interaction with the lunar surface (including magnetic anomalies), is the source of these protons in the near-wake region. Using the entire data from the SWIM sensor of the SARA experiment onboard Chandraya… Show more

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Cited by 13 publications
(31 citation statements)
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“…The velocity distribution of the ions of population “C” in the solar wind rest frame, where the velocities are resolved into components parallel to B IMF ( v ∥ ) and perpendicular to B IMF ( v ⊥ ) (similar to the method discussed in Dhanya et al []) is shown Figure d. For reference, the velocity distribution of the actual solar wind at the location of the Moon (time‐shifted ACE data) is also shown in Figure d (asterisk symbol) in aLSE coordinates.…”
Section: Observationmentioning
confidence: 67%
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“…The velocity distribution of the ions of population “C” in the solar wind rest frame, where the velocities are resolved into components parallel to B IMF ( v ∥ ) and perpendicular to B IMF ( v ⊥ ) (similar to the method discussed in Dhanya et al []) is shown Figure d. For reference, the velocity distribution of the actual solar wind at the location of the Moon (time‐shifted ACE data) is also shown in Figure d (asterisk symbol) in aLSE coordinates.…”
Section: Observationmentioning
confidence: 67%
“…The pixel size is 7.6° full width at half maximum in elevation direction and varies from 6.4° to 17.6° full width at half maximum in azimuthal direction, depending on viewing direction. Assisted by the nadir‐pointing spacecraft motion, the FOV covers ∼2 π within half of the orbit (more details about SWIM are provided in Futaana et al [], Bhardwaj et al [], and Dhanya et al [, ]).…”
Section: Instrumentation and Data Sourcesmentioning
confidence: 99%
“…For the upstream solar wind plasma parameters, such as solar wind velocity and IMF, level‐2 data of the solar wind electron, proton, and alpha monitor (SWEPAM), and magnetometer (MAG) instruments onboard the Advanced Composition Explorer (ACE) satellite are used. Since ACE makes measurements at the L1 point of Sun‐Earth system, we time shifted the solar wind parameters to the location of the Moon (Dhanya et al, ). The convective electric field (CEF) of the solar wind is derived from the solar wind velocity ( V s w ) and IMF ( B I M F ) as trueEc=trueVsw×trueBIMF.…”
Section: Instrument and Datamentioning
confidence: 99%
“…The indirect transport include the entry of solar wind scattered from dayside lunar surface to the near wake region (Nishino, Fujimoto, et al, ; Wang et al, ) and also the solar wind scattered from Earth's bow shock (Nishino et al, ). Further, new population of protons is found in the near lunar wake whose source(s) is(are) yet to be identified (Dhanya et al, , ; Vorburger et al, ).…”
Section: Introductionmentioning
confidence: 99%
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