Whenever you see anomalous Hall effect resistivity/conductivity vs. external magnetic field curves, there is always some low-field part with a greater slope that changes to a lesser slope at some characteristic field. In magnets, this low-field region is usually attributed to magnetic domains aligning to the direction of the external field, and the point where the slope changes is called the "saturation magnetization"--this is where all the domains are aligned.
What causes this characteristic field in non-magnetic systems that show the AHE (topological semimetals)?
I.e., What causes the "shoulder" to be at ~1.5 T in this plot of the AHE in ZrTe5--a Dirac semimetal--since it is not magnetic and are therefore no magnetic domains?
