Based on observations of wind vector above Tanziling mountain of Three Gorges with a three dimensions anemocinemograph, the wind velocity, frequencies of velocity and direction and the daily variation in the areas are analyzed. Combining with the theories of orographic wind and some natural phenomenon,the horizontal characteristics of air flowing filed are given, so the riverway returning breeze is found. It emerged in a river channel around the basic flow if there is a special topographic form. This returning breeze in the areas has a hundred to thousand meter scale. It is different from mountain valley wind directed by Changjiang riverway that it is caused by orographic dynamical factor not by thermodynamical factor and has opposite direction.