Disagree - a cyclonic tornado with an anticyclonic supercell is about as unbelievably rare a tornado you will ever get. First, only about 2-3% of cyclonic storms will produce an anti-cyclonic tornado pair as the RFD bifurcates the updraft and causes a counter-rotating anticyclonic bookend vortex to the right of the main cyclonic vortex. Then, tornadoes from left-moving anticyclonic tornadoes are extremely rare, and have only been documented in the WSR-88D era about a dozen times, if that. What occurred on 5/10/10 in Oklahoma was the left-moving anticyclonic supercell counterpart to what I first describe: The main anticyclonic tornado had a secondary cyclonic vortex on the counter-rotating cyclonic bookend vortex to the *left* of the main anticyclonic vortex/tornado. That left-moving supercell, near Bray, OK, produced two anti-cyclonic tornadoes, one of which spun off a secondary counter-rotating cyclonic tornado. It has never been documented before, and thus is extremely rare.
That all being said, the Taipei tornado is anticyclonic, under an anticyclonic low-level mesocyclone, and a very stout one to say the least. There are WSR-88Ds in Taiwan, so it would be interesting to get a hold of the archived radar data from that event to see if this came from a left-moving supercell.