The cirrus clouds, cirrocumulus clouds, cirrostratus clouds, and cumulonimbus clouds.
The cirrus clouds, cirrocumulus clouds, cirrostratus clouds, and cumulonimbus clouds.
The cirrus clouds, cirrocumulus clouds, cirrostratus clouds, and cumulonimbus clouds.
Clouds are classified into four main categories based on their altitude and appearance: cirrus (high-altitude wispy clouds), cumulus (fluffy clouds with flat bases), stratus (layered clouds covering the sky), and nimbus (dense, dark rain clouds). These categories can further be divided into subcategories based on their specific characteristics and altitude in the atmosphere.
The four prefixes for clouds are cirro-, alto-, strato-, and nimbo-. These prefixes are used to classify different types of clouds based on their altitude and characteristics.
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There are generally four main types of clouds: cirrus, cumulus, stratus, and nimbus. Each type is classified based on its appearance and altitude within the atmosphere.
The four general families of clouds are cirrus (high-level clouds), cumulus (mid-level clouds), stratus (low-level clouds), and nimbus (vertical clouds that produce precipitation). Each family is categorized based on their appearance and altitude in the atmosphere.
Stratus -- very low on ground level, fog Cumulus -- sunny day clouds, low in the sky Cumulonimbus -- they extend through all levels Cirrus -- ice clouds, the highest clouds Sixty years ago I was taught in school the above were the types of clouds, but apparently it isn't that simple. Visit the link below to understand cloud types more thoroughly.
The four basic cloud families are cirrus (high-altitude, wispy clouds), cumulus (puffy, cotton-like clouds), stratus (layered clouds covering the sky), and nimbus (rain-bearing clouds). Each family has variations and different cloud types within it.
Four Steps in the Clouds was created in 1942.
The troposphere. The troposphere is one of the four layers of the atmosphere (0-10km in altitude) containing water vapour. Clouds are formed by water condensing and as air cools. This is why cloud formation is possible because the temperature of the troposphere decreases with altitude.
The four classes of titration are acid-base titrations, redox titrations, complexometric titrations, and precipitation titrations. These classes are based on the type of reaction that occurs during the titration process and the corresponding indicators used to determine the endpoint.