VEX coordinates (in RV) at the time of its crossing (in UT) during an entry and exit (third to fifth columns) through a plasma structure within the Venus wake. Values for the density (cm−3) and speed v (km/s) of planetary O+ ions together with their kinetic energy density ρv2 (10−10 ergs/cm−3) are given in the sixth to eight columns, and the last column has the time width of the vortex structure measured between the inbound and the outbound crossings (the segment between x = −2.30 RV and x = −1.95 RV is the same for both the sept 21–2009 and the sept 26–2009 orbits).
Measurements conducted with the Venus Express (VEX) spacecraft at its entry and exit through vortex structures in the Venus wake reveal that their position varies with the solar cycle. Both crossings are consistently measured closer to Venus during minimum solar cycle conditions and are gradually encountered at larger distances downstream from the planet along the solar cycle. At the same time their width along the VEX trajectory on the plane transverse to the solar wind direction is larger during minimum solar cycle conditions and show a gradual decrease along the solar cycle. As a result the vortex structures are envisioned as features that gradually become thinner as they extend along the Venus wake and agree with the geometry of a vortex flow in fluid dynamics whose thickness decreases with the downstream distance from an obstacle. Similar conditions should also be applicable to Mars and other bodies within the solar system and also possibly to exo-planets in external stellar systems.
- Venus Wake
- Vortex Structures
- Pressure Balance Conditions
Measurements conducted with various spacecraft across the Venus wake: the Mariner 5, the Venera, the Pioneer Venus Orbiter (PVO), and the Venus Express (VEX) spacecraft have provided evidence of plasma features that resemble vortex structures in fluid dynamic problems. It has been noted that the anti-solar directed flow of the plasma particles in the Venus wake is rotated to even become oriented back to Venus. The early measurement of that effect was reported by Pérez-de-Tejada et al. [1, 2, 3] from the PVO plasma data and that gave place to conditions that could be assessed as resulting from a vortex structure. Further information on the observation of vortex structures in the Venus wake was reported by Lundin et al. [4, 5] from measurements conducted with the ASPERA instrument onboard VEX. In this case it was possible to identify the scale size and position of vortex structures with information on the distribution of the velocity vectors of the solar wind and planetary ions that stream within and around those features.
A general view of the shape of a vortex structure is reproduced in the left panel of Figure 1 showing in the plane transverse to the solar wind direction a vortex structure with a scale size comparable to that of the planet with a circulation sense that is counterclockwise when seen from the wake back to Venus. A circulation pattern of the solar wind direction in cylindrical coordinates along the Venus wake is added in the right side panel of Figure 1 with indications of a sunward directed flow return in the central wake. Comparable variations in the plasma velocity vector have also been recently reported from the VEX measurements . Different from that motion there has also been information derived from the PVO and VEX measurements on an east–west displacement of planetary ion fluxes and that leads to the overall deflection of the trans-terminator ionospheric flow toward the dawn-hemisphere as it moves into the night-side (, see Fig. 15; , see Fig. 7b). A deflection in that direction can be accounted for in terms of the fluid dynamic Magnus force produced by the joint contribution of the unidirectional solar wind velocity and the rotation of the Venus atmosphere/ionosphere [8, 9].
2. Vortex structures
Ample information on the speed and density values of the solar wind and planetary ions is their energy spectra obtained with the ASPERA instrument onboard the VEX spacecraft. A suitable example is provided by the data of the Sept. 26–2009 orbit reproduced in Figure 2 and that probed by the near vicinity of the midnight plane (small Y-values shown at the bottom of the figure). The energy spectra of the O+ ion component (second panel) exhibit variations that indicate the presence of appreciable planetary O+ ion fluxes between 02:05 UT and 02:30 UT and that lead to enhanced values of their density and speed (third and fifth panels). At the same time the magnetic field intensity exhibits decreased values within that time interval with an oscillating response of its components (seventh panel). The later indicates the possible presence of a vortex structure within the region where enhanced values of the density and speed of the O+ ion fluxes are clearly distinguished. An important property of the observed values is that the kinetic energy density of such fluxes (mnv2 ~ 10 10−10 ergs cm−3) is comparable to the magnetic energy density (B2/8π ~ 4 10−10 ergs cm−3) measured in the vicinity of that region where B ≈ 10 nT. As a result a near pressure balance condition between values measured outside is suggested within a region with evidence of a vortex structure. It is to be noted that these variations occurred far downstream from the planet (by X < −1.70 RV with this latter parameter being the Venus radius) and thus are unrelated to the crossing of the VEX spacecraft near the Venus ionosphere where X ≈ 0 (X, Y, and Z represent Cartesian coordinates indicating, respectively, the Venus-sun direction, the direction opposite to the motion of Venus around the sun, and the axis transverse to the plane formed by both vectors).
Similar conditions have also been identified in other VEX orbits that were traced by the vicinity of the midnight plane and that exhibit as well a near pressure balance condition between the region where enhanced density and speed values of the planetary ions are measured with the magnetic energy density of the magnetic fluxes encountered in their vicinity . At the same time there is no evidence of a sudden and strong reversal in the direction of the Bx magnetic field component as it would be expected across a plasma sheet embedded by the middle of the wake. On the contrary the enhanced values of the density of the O+ ion population measured by the vortex structure indicates that there is not a local plasma expansion in that region.
3. Distribution of vortex structures in the Venus wake
Different from those properties it is necessary to examine changes of the vortex structures in their position along the nearly 8 years of observations conducted with the VEX spacecraft (between 2006 and 2013). A quantitative analysis of their location was made when VEX entered and exited those structures that was derived from the energy spectra of the planetary ions in the 20 VEX orbits listed in Table 1 . A comparative view of the distribution of the vortex structures on the XZ plane of the solar wind velocity direction is presented in Figure 3 to show the position of the VEX entry and exit crossings in orbits that probed near the midnight plane. Two sets with 4 orbits corresponding to measurements made in 2006 and in 2009 indicate a different displacement of the vortex structures in the Z-direction. There is a general preference of those features to occur closer to Venus in the 2009 measurements since their passage across the Z = 0 axis is by X = −1.7 RV in that set while it reaches X = −2.2 RV in the 2006 measurements. This difference implies that the vortex structures are located closer to Venus during solar cycle minimum conditions by 2009 and that their position along the wake varies during that cycle.
A more extended description of the position and geometry of the vortex structures implied by the data of the orbits listed in Table 1 is depicted in Figure 4 to show changes in their location and extent during 8 years of VEX operation. In particular, they describe variations in their width as follows: For each orbit there is a segment bounded by the entry and exit of the spacecraft with a number that marks the two last digits of the year when measurements were made (they include the 4 orbits for 2006 and 4 for 2009 that were discussed in Figure 3 ). Most notable is that the segments identify 2 different regions; one corresponding to orbits before the minimum solar cycle conditions (between 2006 and 2009) and the other to orbits that occurred during and after those conditions (between 2009 and 2013). Two big circles select schematically different set of orbits that are located either far away from Venus between 2006 and 2009 (left circle) and those that are placed closer to Venus between 2009 and 2013 (right circle) during solar cycle minimum conditions. The implication here is that as in Figure 3 vortex structures occur closer to Venus during minimum solar cycle conditions.
Equally notable is that the time width ΔT (segment length) in the 2006–2009 orbit range is clearly smaller (placed at lower values along the vertical coordinate within the left circle) than that in the 2009–2013 orbit range (larger values in the right circle). As a result the thickness of the vortex structures located far away from Venus (left circle) becomes smaller with increasing distance along the wake thus implying that like in a corkscrew flow they thin out with distance downstream from Venus.
A schematic view of a corkscrew vortex flow structure in fluid dynamics is illustrated in Figure 5 to represent the equivalent geometry of a similar structure in the Venus wake and that is formed by the distribution of planetary O+ ions eroded by the solar wind from the Venus ionosphere
4. Conditions applicable to other planets
The main output of these concepts is that the position of the vortex structures along the Venus wake and their width measured along the VEX trajectory vary along the solar cycle thus implying a continuous displacement of the region where they apply. Similar conditions should also be applicable along the plasma wake of other planets and satellites within the solar system and may as well reach those suitable to exo-planets impacted by stellar winds.
Throughout the solar system the most likely candidates are Venus and Mars which do not have a strong intrinsic magnetic field that deflects the solar wind before it reaches their upper atmosphere
The fluid dynamic response of the solar wind that interacts with planetary ionospheres is ultimately produced by wave-particle interactions inferred from the observation of frequent oscillations in magnetic field profiles measured in the Venus wake [16, 17, 18]. As a whole such interactions provide a mechanism to transfer momentum between both ion populations and thus erode the upper layers of the Venus ionosphere . That process implies in turn local plasma heating [19, see Fig. 35; 20, 21] and the removal of ionospheric plasma in the form of channels or ducts that extend downstream along the Venus wake [22, 23]. These various features are in agreement with phenomena observed in fluid dynamic problems and provide an account of measurements conducted in the Venus wake with various spacecraft. The identification of vortex structures in the Venus wake whose position and width varies during the solar cycle provides a remarkable result that justifies the importance of the fluid dynamic approach.
We wish to thank Gilberto A. Casillas for technical work provided. Financial support was available from the INAM-IN108814-3 Project.