stratus cloud การใช้
- Stratus clouds may produce a light drizzle or a small amount of snow.
- Once the temperature drops below the dew point, a stratus cloud can form.
- These velocities are common in convective downdrafts, but are not typical for stratus clouds.
- Stratus clouds are layered and cover most of the sky.
- As temperatures drop after sunset, the marine layer deepens and coastal stratus clouds thicken.
- Ocean fog and stratus clouds will lap against the Middle Atlantic and New England shores.
- A "'sea of fog "'is formed from stratus clouds or fog and does not show undulations.
- Stratus cloud, which probably dominated during some of the glaciations would have provided insulation but little precipitation.
- Low stratus clouds dulled the southern California coast Thursday as Pacific moisture condensed over chilly coastal waters.
- Low stratus clouds lay over the Ocksenkopf.
- Stratus clouds are thin, flat, fog-like layers.
- Stratus clouds are too low to produce virga, or rain shears that evaporate before reaching the ground.
- For example, middle cumulus clouds are called " altocumulus " and high stratus clouds are " cirrostratus ."
- Humidity can then reach saturation and condensation leads to a very uniform stratocumulus cloud, stratus cloud or fog.
- Early summers can often bring cool, overcast weather ( fog and low stratus clouds ) to coastal California.
- When stratus clouds are very thick, they become dark nimbostratus clouds, which can produce rain, drizzle or snow.
- The frequency of fog and low-lying stratus clouds is due to a combination of factors particular to the region.
- The low, sharp inversion can lead to areas of persistent stratocumulus or stratus cloud, colloquially known as anticyclonic gloom.
- Stratus clouds don't produce accessory clouds, but a supplementary feature "'praecipitatio "'is derived from Latin, which means " precipitation ".
- Low stratus clouds dulled the Southern California coast the last several mornings as Pacific moisture condensed over chilly coastal waters.
- ตัวอย่างการใช้เพิ่มเติม: 1 2 3