There are 4 types of clouds namely cirrous,cumulus ,nimbus and another one cloud(which is very black)
out of these cirrous clouds are the bright white clouds which u can see in morning during sunny days.
Not all clouds are pure white, however, for those that are white, it is due to their altitude and the reflection of sunlight. For example, a cirrus cloud has an altitude of approximately 8km above sea level. At such extreme altitudes all high-level clouds are made up only of ice crystals, as the water vapor from which they are initially formed has frozen. The ice crystals reflect sunlight. When flying above clouds during the day, they are always bright white. When we get dark clouds, they are so thick that they soak up most of the sunlight or reflect it upwards, and so things aren't as bright below. Storm clouds are the thickest clouds, and look the darkest from down below, though they still look bright white if we see them from above. Gray color of the clouds is caused by higher clouds casting their shadow on lower-based clouds, or that the clouds are so dense that their top parts absorb most of the sunlight, casting their own shadow along their base, making them dark on the bottom.
snow clouds
White fluffy clouds, known as cumulus clouds, do not bring rain on their own. Rain typically falls from higher-level clouds such as nimbostratus or cumulonimbus clouds, which have more moisture and larger vertical development. Cumulus clouds may eventually develop into rain-producing clouds if they continue to grow and merge with other clouds.
Yes
Dark clouds are usually associated with precipitation and thunderstorms, containing high levels of moisture and turbulence. In contrast, white clouds are typically associated with fair weather and consist of water droplets or ice crystals. Dark clouds tend to block more sunlight and can result in cooler temperatures compared to white clouds.
White is a bright, neutral color often associated with purity, cleanliness, and simplicity. It reflects light and is typical of snow, clouds, and white sand.
You would likely see cumulus clouds on a bright sunny day. Cumulus clouds are fluffy, white clouds with a flat base and rounded tops that form due to rising air currents. They do not bring precipitation and are often associated with fair weather.
Not all clouds are pure white, however, for those that are white, it is due to their altitude and the reflection of sunlight. For example, a cirrus cloud has an altitude of approximately 8km above sea level. At such extreme altitudes all high-level clouds are made up only of ice crystals, as the water vapor from which they are initially formed has frozen. The ice crystals reflect sunlight. When flying above clouds during the day, they are always bright white. When we get dark clouds, they are so thick that they soak up most of the sunlight or reflect it upwards, and so things aren't as bright below. Storm clouds are the thickest clouds, and look the darkest from down below, though they still look bright white if we see them from above. Gray color of the clouds is caused by higher clouds casting their shadow on lower-based clouds, or that the clouds are so dense that their top parts absorb most of the sunlight, casting their own shadow along their base, making them dark on the bottom.
In science, "puffy white clouds" are known as cumulus clouds.
Angels, clouds, god, bright light, pearly gates, and white clothes.
All clouds are white, meaning the water droplets that make up a cloud scatter light in all wavelengths so they combine to produce white light. Clouds appear dark if they are in the shadow of other clouds or, sometimes, if the top of the same cloud produces a shadow on itself. There is also a darker look to some clouds if the background color is bright sunlight, making a great contrast.
Bright, No clouds, Nice weather
White Fluffy Clouds was created in 2003.
blue dark spot white bands of white clouds some white clouds
snow clouds
Cumulus clouds are the pig puffy white clouds.
Cold-air clouds, such as cumulus and stratocumulus clouds, are made up of tiny water droplets or ice crystals suspended in the air. These clouds typically form at low altitudes and are associated with stable atmospheric conditions. The cloud droplets or ice crystals in cold-air clouds are much smaller compared to those in rain clouds, which is why they often appear bright white.