fog
Condensed water droplets held suspended in the air are known as fog. Fog forms when the air near the ground becomes saturated with water vapor, causing the water vapor to condense into tiny droplets that linger in the air.
When clouds come near the land, it is called fog. Fog is a visible aerosol consisting of tiny water droplets suspended in the air, usually observed near the ground.
A cloud at ground level that reduces visibility is known as fog. It forms when air near the ground cools to the point where it can no longer hold all its moisture, causing the water vapor to condense into tiny water droplets that stay suspended in the air. Fog is common near bodies of water or in areas with high humidity.
Fog is a type of cloud that forms near the ground. It occurs when air near the surface cools to the point where it can no longer hold its water vapor, causing it to condense into tiny water droplets.
Condensation near the ground is commonly referred to as "fog." It occurs when water vapor in the air cools and condenses into tiny water droplets, reducing visibility. Fog typically forms in calm, humid conditions, especially during the night or early morning when temperatures drop.
Condensed water droplets held suspended in the air are known as fog. Fog forms when the air near the ground becomes saturated with water vapor, causing the water vapor to condense into tiny droplets that linger in the air.
fog because its made up of little water droplets
A collection of water droplets suspended in the air is called a cloud. If the collection of water droplets is close to the ground it is called fog.
When clouds come near the land, it is called fog. Fog is a visible aerosol consisting of tiny water droplets suspended in the air, usually observed near the ground.
Clouds that form very near the ground are called fog. Fog consists of suspended water droplets or ice crystals that reduce visibility and can form when moist air comes into contact with a cooler surface.
A stratus cloud that forms near the ground is known as fog. Fog consists of water droplets suspended in the air close to the Earth's surface, resulting in reduced visibility. It typically forms when the air near the ground cools to the point where it can no longer hold all of its moisture.
These are most likely mist or drizzle. Mist consists of tiny water droplets suspended in the air near the ground, while drizzle is very light rain with small droplets that fall slowly and steadily. Both mist and drizzle are common in humid or foggy conditions.
When air is cooled to the dew point near the ground, it forms a stratus cloud called fog. In foggy conditions, visibility is significantly reduced due to the water droplets suspended in the air near the surface.
fog
persepitation
A cloud at ground level that reduces visibility is known as fog. It forms when air near the ground cools to the point where it can no longer hold all its moisture, causing the water vapor to condense into tiny water droplets that stay suspended in the air. Fog is common near bodies of water or in areas with high humidity.
A stratus cloud that forms near the ground is known as fog. Fog is essentially a stratus cloud that develops at the Earth's surface, reducing visibility due to suspended water droplets or ice crystals. It often forms when the air near the ground cools to the point where it can no longer hold its moisture content.