The influence of different time-scale circulations on the sudden track of the Typhoon Goni (1515) was analyzed by filtering the synoptic-scale, QBWO (Quasi-Biweekly Oscillation), and MJO (Madden-Julian Oscillation) circulation fields from FNL wind field data. The moving path of Goni can be divided into three stages, and the sudden track appeared in the second stage. In the first stage, the anti-cyclone east to Goni in synoptic-scale circulation and the wave train in QBWO circulation field lead the cyclone to move towards northwest. The effect of the steering flow in MJO circulation is weak. In the second stage, the anti-cyclone east to Goni in synoptic-scale circulation and the cyclone in low-frequency circulation field promote a sudden transition with a right angle of the cyclone. The synoptic-scale propagation leads Goni to transfer northward, and the low-frequency propagation leads Goni to transfer eastward. In the third stage, the anti-cyclone and the cyclone in synoptic-scale circulation field, the anti-cyclone in QBWO circulation field and the ridge in MJO circulation field lead the cyclone to move northeast. The easterly wind from the cyclone in MJO circulation field lead Goni to move westward, but Goni still moves eastward because the easterly wind is negated by strong westerly wind in synoptic-scale circulation field.