What do nimbostratus clouds produce

Nimbostratus clouds typically occur in advance of the front and trigger warmer temperatures. Winds are typically light and variable beneath a layer of nimbostratus clouds. Precipitation is generally light or moderate and is widespread. In winter, precipitation can be snow or sleet. Because of the slow movement of warm fronts, this precipitation can last hours or days, greatly reducing visibility.

Cold air masses are denser than an advancing warm front. As a result, the cold air must retreat to make room for the warm, moist air.

Sometimes the cold air mass resists this gentle push. When this occurs, the warm front can advance very slowly, leading to days of rainy weather. Geographical features can contribute to this resistance. They are similar to altostratus in this way. Nimbostratus clouds. Height of base: 2, - 10, ft Shape: Bands or areas of individual cells Latin: nimbus - rainy cloud; stratus - flattened or spread out Precipitation: Continuous rain or snow likely What are nimbostratus clouds?

How do nimbostratus clouds form? What weather is associated with nimbostratus clouds? Nimbostratus Cloud Facts. Light gray to very dark gray. Cloudy to mostly cloudy.

Nimbostratus Cloud Species. Nimbostratus Cloud Varieties. Nimbostratus Cloud Supplementary Features. Nimbostratus clouds have two associated supplementary features: praecipitatio and virga. Precipitation reaching the surface. Latent Heat. Levanter cloud. Lightning strike. Millibar and hectopascal. NOAA satellites. North Atlantic Drift Gulf Stream.

Polar Orbiting Satellites. Polar low - the arctic hurricane. Precipitation Map. Rain gauge. Roll cloud. Rotor cloud. Saffir-Simpson scales. Sc duplicatus. Sc perlucidus. Sc undulatus. Shelf Cloud. Sometimes a bit fishy. Southern Oscillation. Swithun's Day. Standard Reference Period. Stevenson Screen. Sun pillar. Supercooled clouds. Surface wind. Thunderstorm Probability. Tornado Alley. Troposphere - Diagram. UV Index. Ultraviolet radiation. Virga or Fallstreak.

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