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Digital atmosphere from weather graphics download#
The photo was taken from a viewpoint that was at an angle from the vertical, rather than looking straight down towards the Earth’s surface.
The cloud tops flatten and spread into an anvil shape, as illustrated by this astronaut photograph. The tropopause halts further upward motion of the cloud mass. Beyond the tropopause, the air no longer gets colder as altitude increases. The tropopause is characterized by a strong temperature inversion. If enough moisture is present to condense and heat the cloud mass through several convective cycles, a tower can rise to altitudes of approximately 10 kilometers at high latitudes and to 20 kilometers in the tropics before encountering a region of the atmosphere known as the tropopause-the boundary between the troposphere and the stratosphere. This leads to the characteristic vertical “towers” associated with cumulonimbus clouds, an excellent example of which is visible in this astronaut photograph. This type of convection is common in tropical latitudes year-round and during the summer season at higher latitudes.Īs water in the rising air mass condenses and changes from a gas to a liquid state, it releases energy to its surroundings, further heating the surrounding air and leading to more convection and rising of the cloud mass to higher altitudes. The air mass itself also expands and cools as it rises due to decreasing atmospheric pressure, a process known as adiabatic cooling. Surface air is warmed by the sun-heated ground surface and rises if sufficient atmospheric moisture is present, water droplets will condense as the air mass encounters cooler air at higher altitudes. Perhaps the most impressive of cloud formations, cumulonimbus (from the Latin for “pile” and “rain cloud”) clouds form due to vigorous convection (rising and overturning) of warm, moist and unstable air.
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