Which feature is NOT typically associated with maritime air masses?

Maritime air masses are characterized by their formation over oceans or large bodies of water, which significantly influences their properties. High humidity is a defining trait of these air masses due to the abundance of moisture evaporating from the water surface. Warm temperatures can also be associated with maritime air masses, particularly in warmer seasons or regions, as the water helps to moderate temperature extremes.

Low stability refers to the tendency of maritime air masses, especially warm ones, to be less stable than continental air masses. This low stability can lead to cloud formation and precipitation due to the presence of moisture and warmer air rising.

In contrast, dry conditions are not typically associated with maritime air masses. Instead, they are moist due to their origin over water. This moisture contributes to the precipitation patterns and weather associated with these air masses. Therefore, the presence of dry conditions stands out as the feature that does not align with the characteristics of maritime air masses.