Stratus Clouds

Stratus clouds are low-level, uniform clouds that typically cover the entire sky like a blanket. They are often gray or white in color and can create overcast or foggy conditions. These clouds are formed when large areas of air are lifted slowly and steadily, causing the air to cool and condense into a continuous layer of clouds.

Characteristics of Stratus Clouds:

1. Appearance: Stratus clouds have a smooth, even, and uniform appearance. They often resemble a gray or white blanket covering the sky.
2. Altitude: Stratus clouds are low-level clouds that usually form at altitudes below 6,500 feet (2,000 meters).
3. Weather: These clouds are associated with overcast skies, light rain, drizzle, or foggy conditions.
4. Formation: Stratus clouds form when air is lifted gradually and steadily, causing it to cool and condense into a continuous layer of clouds.

Study Guide:

When studying stratus clouds, it's important to remember their characteristics and the conditions under which they form. Here are some key points to focus on:

• Describe the appearance of stratus clouds and how they differ from other types of clouds.
• Explain the altitude at which stratus clouds typically form and their association with specific weather conditions.
• Discuss the process of formation for stratus clouds and the role of gradual, steady lifting of air in their creation.

Understanding stratus clouds is essential for learning about weather patterns and cloud formations. Take the time to observe the sky and notice the presence of stratus clouds in different weather conditions.