Can Northwest Pacific Tropical Cyclones Influence the Zonal Movement of the East Asian Mid-Latitude Trough?

Mutual interactions exist between tropical cyclones and the East Asian mid-latitude trough (EAMT). This study mainly used statistical analysis and numerical experiments to :investigate the influence of TCs on the zonal movement of EAMT. Composite results indicate that TCs can induce an average of 11.82 degrees in the EAMT meridional displacement, and the anomalous remote geopotential height (HGT) triggered by TCs serves as an important factor driving the zonal movement of the EAMT. The EAMT tends to move towards the region of negative HGT difference and away from the region of positive HGT difference. The temperature anomalies induced by TCs are a critical factor leading to the HGT anomalies. For the TC Maria case, it induces a maximum meridional displacement of 0.76 degrees of the EAMT at 450 hPa.‌ TC Maria first triggers anomalous cold advection in the mid-latitude regions of the East Asia–Northwest Pacific area, which then leads to an anomalous decrease in HGT within the EAMT trough region under the constraint of hydrostatic equilibrium. Consequently, the anomalous negative HGT caused by the TC results in the zonal movement of the EAMT line. The results of this study provide evidence that remote disturbances induced by TCs in the tropical WNP can affect weather circulation in the mid-latitudes of East Asia.