Abstract Recurving tropical cyclones (TC) in the Western North Pacific can affect the atmospheric circulation over Pacific‐Western North America (PWNA) via interactions with the midlatitude circulation. Using reanalysis and tropical cyclone best‐track data, we examine how recurving TCs that make extratropical transition modulate 500‐hPa ridge characteristics over PWNA during the peak (June‐September) and late (October–December) seasons. TCs recurving at lower latitudes are associated with more intense and poleward‐centered ridges relative to TCs recurving at higher latitudes, and TCs that recurve farther west are associated with relatively westward‐centered ridges. Characteristics of the prevailing midlatitude flow such as its amplitude and positioning relative to the recurving TCs also affect PWNA ridge characteristics, determine whether the flow is amplified or dampened following TC‐midlatitude interactions. Our study highlights multiple factors shaping the diversity of midlatitude circulation responses to recurving TCs, which are relevant for predicting downstream ridge characteristics and their associated surface extremes.