Fluffy Cumulus clouds are formed when bubbles of warm air rise form the Earth's surface. Water vapor the air cools and condenses (turns into liquid) forming clouds droplets. The clouds have a limited depth and are usually short-lived, lasting from 5 to 40 minutes. Sometimes, they develop into rain clouds. They are heapy clouds which form because of surface temperatures rising. When the temperatures rise, also more water (from pipes,etc.) evaporates into the atmosphere and cools off, forming a heapy mass of Cumulus. However, if it is very hot, cumulus clouds can develop even more, forming a Cumulonimbus, a very high storm cloud.
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| - Fluffy Cumulus clouds are formed when bubbles of warm air rise form the Earth's surface. Water vapor the air cools and condenses (turns into liquid) forming clouds droplets. The clouds have a limited depth and are usually short-lived, lasting from 5 to 40 minutes. Sometimes, they develop into rain clouds. They are heapy clouds which form because of surface temperatures rising. When the temperatures rise, also more water (from pipes,etc.) evaporates into the atmosphere and cools off, forming a heapy mass of Cumulus. However, if it is very hot, cumulus clouds can develop even more, forming a Cumulonimbus, a very high storm cloud.
- The Cumulus is the Stage 1 form of the Weather group. It has high magical stats, but low physical ones.
- Please check out Hexadecimal Chart to see what codes are available to name. The hexadecimal code that matches this color is FDFFD5
- Le cumulus est le nuage qui a la forme la plus caractéristique et reconnaissable. Son aspect bourgeonnant le fait, en effet, ressembler à un chou-fleur. On évoque parfois le terme poétique de « moutons nuageux ». Ce nuage est le siège d'un mouvement de convection, similaire à celui qui a lieu dans une casserole d'eau bouillante, constitué d'une colonne d'air ascendant (au cœur du nuage) et de mouvements d'air descendant (à sa périphérie). En s'élevant, l'air subit une détente adiabatique, ce qui refroidit la vapeur d'eau et provoque sa condensation. Au fur et à mesure que le nuage se charge en eau, le cumulus s'étire en hauteur et forme une tour appelée convectus.
- Cumulus (Cu; Latin for heap) is a common genus of cloud which is formed by the rising of pockets of warm air and which has the appearance of a heap of cloud rising from a horizontal base. The cumulus cloud is commonly described as looking like a cotton ball or as "fluffy". Most of the time, cumulus clouds have a solid white colour, but some "towering" cumulus clouds can become dark. Cumulus congestus clouds can develop into cumulonimbus calvus clouds and thence into cumulonimbus incus clouds; each of these is capable of generating storms and showers.
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| - a type of cloud that is becoming a storm cloud but hasn't started storming yet.
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| - Cumulus (Cu; Latin for heap) is a common genus of cloud which is formed by the rising of pockets of warm air and which has the appearance of a heap of cloud rising from a horizontal base. The cumulus cloud is commonly described as looking like a cotton ball or as "fluffy". Most of the time, cumulus clouds have a solid white colour, but some "towering" cumulus clouds can become dark. Cumulus congestus clouds can develop into cumulonimbus calvus clouds and thence into cumulonimbus incus clouds; each of these is capable of generating storms and showers. Cumulus clouds were first described by Luke Howard in 1802 as "convex or conical heaps, increasing upwards from a horizontal base - wool bag clouds".
- Fluffy Cumulus clouds are formed when bubbles of warm air rise form the Earth's surface. Water vapor the air cools and condenses (turns into liquid) forming clouds droplets. The clouds have a limited depth and are usually short-lived, lasting from 5 to 40 minutes. Sometimes, they develop into rain clouds. They are heapy clouds which form because of surface temperatures rising. When the temperatures rise, also more water (from pipes,etc.) evaporates into the atmosphere and cools off, forming a heapy mass of Cumulus. However, if it is very hot, cumulus clouds can develop even more, forming a Cumulonimbus, a very high storm cloud.
- The Cumulus is the Stage 1 form of the Weather group. It has high magical stats, but low physical ones.
- Le cumulus est le nuage qui a la forme la plus caractéristique et reconnaissable. Son aspect bourgeonnant le fait, en effet, ressembler à un chou-fleur. On évoque parfois le terme poétique de « moutons nuageux ». Ce nuage est le siège d'un mouvement de convection, similaire à celui qui a lieu dans une casserole d'eau bouillante, constitué d'une colonne d'air ascendant (au cœur du nuage) et de mouvements d'air descendant (à sa périphérie). En s'élevant, l'air subit une détente adiabatique, ce qui refroidit la vapeur d'eau et provoque sa condensation. Au fur et à mesure que le nuage se charge en eau, le cumulus s'étire en hauteur et forme une tour appelée convectus. Des cumulus peuvent se former dans de nombreux types de situation, mais le cas le plus favorable à leur observation est la situation de traîne après le passage d'une perturbation. Alors que le front froid s'éloigne, le Soleil redevient visible et réchauffe le sol. Par conséquent les basses couches de l'atmosphère se réchauffent par conduction thermique, rendant l'atmosphère instable. Des cumulus isolés bourgeonnent alors ici et là. Dans ces conditions, on dit qu'on a affaire à un « ciel de traîne ».
- Please check out Hexadecimal Chart to see what codes are available to name. The hexadecimal code that matches this color is FDFFD5
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