In two recent posts, we compared an image of the Sun’s far side taken by the Mars rover with the GONG far-side helioseismic map. A large active region is clearly visible in both, though at different apparent locations. This displacement arises solely from differences in viewing geometry. The rover observes the Sun’s far side with distinct values of B0 and L0, which differ from those used in the helioseismic map, and the discrepancies we note result from the combined influence of these parameters. Variations in L0 are driven by the rover’s position in the orbit, which changes over time.
As mentioned earlier, the rover will provide far-side observations for only the next two months. During this period, its viewing angle will gradually shift, yielding perspectives of different portions of the Sun’s far side. Since Mars completes an orbit around the Sun in about 687 days, the Sun's far side can be observed from Mars roughly every other year, with each transit lasting about two months as determined by its orbital velocity.