Stratus Clouds

Stratus clouds are one of the three basic cloud types, alongside cumulus and cirrus clouds. They are low-level clouds that typically form in uniform layers, covering the sky like a blanket. Stratus clouds are generally gray or white in color and can bring overcast or drizzly weather.

Formation of Stratus Clouds

Stratus clouds form when warm, moist air is forced to rise over a large area of cooler air. As the warm air rises, it cools and condenses into a continuous layer of clouds. This process usually occurs in stable, low-pressure conditions.

Characteristics of Stratus Clouds

• Low-level clouds
• Form in uniform layers
• Gray or white in color
• Can bring overcast or drizzly weather

Study Guide

Here are some key points to remember about stratus clouds:

1. Stratus clouds are low-level clouds that form in uniform layers.
2. They are often associated with overcast or drizzly weather.
3. Stratus clouds are important for weather prediction as they can indicate stable atmospheric conditions.
4. Stratus clouds are often found in the mid-latitudes and are less common in tropical and polar regions.

Understanding the formation and characteristics of stratus clouds is essential for meteorology and understanding weather patterns.