Between 30°N and 60°N latitude, the prevailing winds are primarily the westerlies. These winds typically blow from the west to the east and are a result of the Coriolis effect and the temperature differences between the tropics and polar regions.
At lower latitudes (closer to 30°N), winds can also be influenced by the trade winds, which blow from the east toward the west. However, as you move northward toward 60°N, the westerlies become more dominant. This pattern is part of the larger global circulation system, which includes the Hadley cells, Ferrel cells, and polar cells.
In summary, the prevailing winds in the latitudinal zone between 30°N and 60°N are predominantly westerlies, resulting from the mid-latitude atmospheric circulation patterns.