Im not really sure...BUT!.....I know it's either Nimbo or Cirrostatus clouds
Im not really sure...BUT!.....I know it's either Nimbo or Cirrostatus clouds
Cumulonimbus clouds are what heaps of rain clouds are called. Vertical clouds are the heaped up ones, so their names include the root " cumulus." The big, towering storm clouds are called cumulonimbus.
A dark rain cloud is called a nimbus. These clouds produce rain and snow as they are filled with compact and frozen moisture.
Rain-giving clouds are typically referred to as cumulonimbus clouds. These clouds are large, vertically-developed clouds that can produce heavy rain showers, thunderstorms, and even hail.
When rain falls from clouds and freezes along the way, it is called "sleet."
Im not really sure...BUT!.....I know it's either Nimbo or Cirrostatus clouds
Im not really sure...BUT!.....I know it's either Nimbo or Cirrostatus clouds
Clouds in flat layers are called stratus.
Cumulonimbus clouds are what heaps of rain clouds are called. Vertical clouds are the heaped up ones, so their names include the root " cumulus." The big, towering storm clouds are called cumulonimbus.
A dark rain cloud is called a nimbus. These clouds produce rain and snow as they are filled with compact and frozen moisture.
Rain-giving clouds are typically referred to as cumulonimbus clouds. These clouds are large, vertically-developed clouds that can produce heavy rain showers, thunderstorms, and even hail.
When rain falls from clouds and freezes along the way, it is called "sleet."
cirrus
cirrus
Thick low clouds that are a sign of rain are called nimbostratus clouds. These clouds are typically gray and cover the sky, producing long periods of steady precipitation.
Clouds with precipitation are often referred to as nimbostratus clouds. These clouds are characterized by their uniform, thick, gray layers that produce steady rain or snow.
Unbroken layers of low gray clouds that bring light rain, snow, or drizzle are typically associated with stratus clouds. These clouds form in stable atmospheric conditions and cover the sky like a blanket, leading to overcast weather. When the moisture in these clouds condenses, it results in light precipitation, such as drizzle or light snow, often lacking the intensity of heavier rain systems.