Cumulonimbus Clouds Formations Sky Storms Weather Phenomena 22
Definition of Cumulonimbus. Heavy and dense cloud, with a considerable vertical extent, in the form of a mountain or huge towers. At least part of its upper portion is usually smooth, or fibrous or striated, and nearly always flattened; this part often spreads out in the shape of an anvil or vast plume. Under the base of this cloud, which is.
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Cumulonimbus Clouds Formation. Cumulonimbus (from Latin cumulus, "heaped," and nimbus, "rainstorm") is a dense, towering vertical cloud formed by water vapour condensing in the lower troposphere and carried upward by powerful buoyant air currents. Water vapour above the lower portions of the cumulonimbus condenses into ice crystals such.
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This includes strong winds, heavy rain or hail, and thunder and lightning. The name of the cloud also points to the above characteristics. When broken into parts, the name 'cumulonimbus' tells its own story. 'Cumulus' means 'heaped', and 'nimbus' means 'rain-bearing' in Latin. So, in short, a rain-bearing heaped cloud.
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8.1 Introduction. The cumulonimbus cloud, or thunderstorm, is a convective cloud or cloud system that produces rainfall and lightning. It often produces large hail, severe wind gusts, tornadoes, and heavy rainfall. Many regions of the earth depend almost totally upon cumulonimbus clouds for rainfall.
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1. Learn how clouds form Looking up at the sky you've probably noticed clouds. While clouds are similar in many ways, there are lots of different types and they form in different ways. Learn more about clouds and how they form on NASA Climate Kids. 2. Learn about types of clouds
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How Are Clouds Classified? Clouds get classified according to the altitude at which they form, their upper height, and their shape. The names come from Latin words. Four common types are cumulus, stratus, nimbus, and cirrus.
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What Is A Cumulonimbus Cloud? When water vapor is drawn upwards by strong air currents, it can represent the developmental stage of a cumulonimbus cloud. The weather conditions necessary for such clouds to form include an unstable air mass, sufficient moisture, and an upward force (typically provided by heat). An example of cumulonimbus cloud.
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Small cumulus are commonly grouped with the low clouds because they do not show significant vertical extent. Of the multi-level genus-types, those with the greatest convective activity are often grouped separately as towering vertical. The genus types all have Latin names. The genera are also grouped into five physical forms.
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What are clouds? Clouds are "a visible mass of particles of condensed vapor (such as water or ice) suspended in the atmosphere of a planet (such as the earth) or moon." According to Merriam-Webster
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Cumulonimbus (from Latin cumulus 'heaped', and nimbus 'rainstorm') is a dense, towering vertical cloud, [1] typically forming from water vapor condensing in the lower troposphere that builds upward carried by powerful buoyant air currents.
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Cumulonimbus storms are the most dramatic of cloud features, and are a vital component in the atmospheric circulation. Individual cumulonimbus cells occur on horizontal scales of around 10 km and commonly extend to the tropopause, over a timescale of an hour or so (Figure 3).However, it is common for cumulonimbus systems to self-organize into an MCS with a significantly longer life cycle.
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Latin: cumulus - heap; nimbus - rain cloud; Precipitation: heavy rain and thunderstorms; What are cumulonimbus clouds? Cumulonimbus clouds are menacing looking multi-level clouds, extending high into the sky in towers or plumes. More commonly known as thunderclouds, cumulonimbus is the only cloud type that can produce hail, thunder and.
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The fan-shaped cloud in the center of this picture is the edge of a cumulonimbus anvil visible through lower level cumulus clouds. This is a fairly common sight out West, but is rarely seen in the East due to the fact that the very moist atmosphere around a thunderstorm often obscures any detail of the clouds. Photo by Jeff Caplan, NASA.
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Clouds are visible accumulations of tiny water droplets or ice crystals in the Earth's atmosphere. Clouds differ greatly in size, shape, and color. They can appear thin and wispy, or bulky and lumpy. Clouds usually appear white because the tiny water droplets inside them are tightly packed, reflecting most of the sunlight that hits them.