In this work, we investigate the interhemispheric transpolar arc (TPA) conjugacy using four previously published datasets based on Polar UV images, DMSP particle data, and IMAGE images, and a new TPA list based on DMSP SSUSI images during 1 Sep to 15 Oct 2015. IMF Bx ${B}_{\mathrm{x}}$ and the Earth's dipole tilt have often been suggested to influence the TPA conjugacy, as both induce a north‐south asymmetry on the magnetosphere. However, by comparing these parameters at TPA formation with the background distribution for each dataset, we find that neither the dipole tilt nor Bx ${B}_{\mathrm{x}}$ plays a major role for the TPA conjugacy in four of the five datasets. The well‐known correlation between initial TPA location and IMF By ${B}_{\mathrm{y}}$ appears in all datasets with information about the TPA formation. In addition, we find that a minority of dawnside TPAs form during the “wrong” By ${B}_{\mathrm{y}}$ sign. In the northern (southern) hemisphere, dawn TPAs appear also during weakly duskward (dawnward) IMF. Due to the polar orbit of DMSP satellites, TPA conjugacy and location can be examined on a case‐by‐case basis with the new dataset. The results show that at least 73% of TPAs appear in both hemispheres simultaneously. IMF Bx ${B}_{\mathrm{x}}$ and dipole tilt values for conjugate TPAs do not differ from those for non‐conjugate TPAs. Most conjugate (isolated) TPAs appear on opposite oval sides in each hemisphere (57%). Interestingly, in case northern and southern hemisphere TPAs form on the same oval side, they appear typically at dawn during weak IMF By ${B}_{\mathrm{y}}$.