Peculiarities of the spatial distribution of the begin� nings and the most intense stages of tropical cyclones in the northwestern part of the Pacific Ocean are dem� onstrated in this paper in comparison with the values of the gravity force anomalies in the cyclone zone. Relations are distinguished in which some group char� acteristics of the tropical cyclones and the spatially average values of the gravity force anomalies are for� mally inversely related. On the basis of these results, the supposition that gravity force anomalies can to some extent influence the cyclonic regime in the study region is put forward. The author is not familiar with any special empiri� cal (detailed) investigations on the role of gravity force anomalies (GFAs) in the life of tropical cyclones. It is likely that in monographs [1, 2] the influence of the GFAs on the hydrometeorological processes is investi� gated for the first time. There are also sections dedi� cated to tropical cyclones. Here, the tropical cyclones are only one of the phenomena that illustrate the validity of the ideas and research methods described in the monographs. Therefore, only general words are said about the influence of the GFAs. Publication [3] is also dedicated to research into gravity force anoma� lies. However, here, as well as in the previous publica� tions of this author, the role of the GFA is predomi� nantly studied in the Antarctic region. Quite large ter� ritories are considered, and only general estimates of the GFA level are given for the entire territory. This approach to estimates of the influence of GFAs is cor� rect in the analysis of extratropical cyclones, taking into account their size. The sizes of the tropical cyclones are significantly