Air masses that form over the ocean near the poles have \( \text{ } \) warm moist air cold moist air

Cold moist air is the characteristic of air masses that form over the ocean near the poles. These air masses, known as polar maritime air, are generally cool and can bring significant precipitation when they move towards lower latitudes, influencing weather patterns and climates. When these cold moist air masses collide with warmer land masses, they can lead to dramatic weather phenomena, such as storms or heavy rainfalls. This interaction is a key factor in weather forecasting and understanding climate variations in coastal regions. So, next time you’re caught in a sudden downpour, you might just have one of these chilly air masses to blame!