nimbostratus造句

• Precipitation commonly becomes heavier and more widespread if it thickens into nimbostratus.
• Though found worldwide, nimbostratus occurs more commonly in the middle latitudes.
• As it cools, any water vapor that is present will nimbostratus.
• The nimbostratus are flat; the cumulonimbus are puffy.
• Nimbostratus usually has a thickness of about 2000 m.
• Clouds of the genus nimbostratus tend to bring constant precipitation and low visibility.
• Fractonimbus may eventually merge completely with overlying nimbostratus clouds.
• However, an advancing nimbostratus cloud could have a diffuse precipitation leading edge.
• Nimbostratus and cumulonimbus clouds are rain clouds and are usually darker than other clouds.
• Frontal precipitation typically falls out of nimbostratus clouds.
• The top of a nimbostratus deck is usually in the middle level of the troposphere.
• Nimbostratus cloud droplets can also be quite large, up to 0.015 mm radius.
• If the precipitation increases in persistence and intensity, the altostratus cloud may thicken into nimbostratus.
• They comprise two or three genera depending on the system of height classification being used : nimbostratus.
• These are the nimbostratus clouds, and the cumulonimbus clouds, and are classified as pannus clouds.
• This sometimes leads to the continued exclusion of nimbostratus from the group of vertical clouds by some independent meteorologists.
• Lightning from an embedded cumulonimbus cloud may interact with the nimbostratus but only in the immediate area around it.
• Altostratus tends to form ahead of a warm or occluded front, the altostratus gradually thickening into rain bearing nimbostratus.
• The occurrence of cumulonimbus and nimbostratus together is uncommon, and usually only nimbostratus is found at a warm front.
• The occurrence of cumulonimbus and nimbostratus together is uncommon, and usually only nimbostratus is found at a warm front.