Table of Contents
- What process causes clouds to form?
- How do clouds form by convection?
- What is the difference between white clouds and black clouds?
- What are the 4 clouds?
- Why is the Colour of sky is blue?
- Why is the sky pink?
- Does a pink sky mean pollution?
Nimbostratus clouds
What process causes clouds to form?
Clouds form when the invisible water vapor in the air condenses into visible water droplets or ice crystals. For this to happen, the parcel of air must be saturated, i.e. unable to hold all the water it contains in vapor form, so it starts to condense into a liquid or solid form.
How do clouds form by convection?
Convection refers to air rising vertically in the atmosphere due to heating. Advection is the horizontal transfer of air that usually results in warmer air being forced up over cooler air. Both advection and convection results in the formation of clouds. Cumulus clouds tend to form in unstable atmospheres.
What is the difference between white clouds and black clouds?
The parts where the sunlight passes through it are white, while those that receive less light have a darker gray color to it. Clouds that become big enough to have gray spots are because they have become so big that less light can pass through the bottom or base area.
The Four Core Types of Clouds
- Cirro-form. The Latin word ‘cirro’ means curl of hair.
- Cumulo-form. Generally detached clouds, they look like white fluffy cotton balls.
- Strato-form. From the Latin word for ‘layer’ these clouds are usually broad and fairly wide spread appearing like a blanket.
- Nimbo-form.
Why is the Colour of sky is blue?
The Short Answer: Gases and particles in Earth’s atmosphere scatter sunlight in all directions. Blue light is scattered more than other colors because it travels as shorter, smaller waves. This is why we see a blue sky most of the time.
Why is the sky pink?
The phenomenon of scattering is also why the sky turns red, orange, and pink at sunset. The science is the same, with short-wavelength blue and violet light scattered by molecules in the atmosphere while longer-wavelength red, orange, and pink light passing through and hitting the clouds.
Does a pink sky mean pollution?
Similarly, the vibrant oranges and reds of “clean” sunsets give way to pale yellows and pinks when dust and haze fill the air. But airborne pollutants do more than soften sky colors. They also enhance the attenuation of both direct and scattered light, especially when the sun is low in the sky.
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Depending on your perspective and your situation, few sights in nature are quite so foreboding as a black-bellied cloud looming on the horizon. A picnicker or baseball player doesn’t like the looks of it, but a farmer surveying her thirsty field probably does. Rain-bearing clouds such as nimbostratus and cumulonimbus (also called thunderheads) classically show these heavy gray or nearly black bases, but non-precipitating clouds of sufficient depth – or those cast in shadow – can also exhibit dark undersides.
A Little Background: The Composition of Clouds
To talk about the color variation of clouds, we need to understand their basic composition. Clouds form when moist air parcels cool enough for their water vapor to condense into droplets, which may occur when heated air rises into the atmosphere, for example, or when an air mass shoves up over a mountain. If the temperature is cold enough, a cloud may also create ice crystals. If these droplets and/or crystals grow large enough in size – by merging with one another, basically – they may become too heavy to remain aloft and fall as precipitation: rain, snow, hail or graupel.
The Latin word nimbus means “dark cloud” or “rain storm,” and meteorologists use it to classify two of the major types of rain-bearing clouds: nimbostratus, layered rain clouds that don’t produce lightning, and cumulonimbus, deep cumulus clouds generating lightning, thunder and heavy downpours.
Sunlight and Cloud Cover
A clear sky during daytime appears blue because its tiny atmospheric molecules and particles selectively scatter the short blue wavelength of visible light. The water droplets and ice crystals of a cloud, while still miniscule to the naked eye, are larger than those atmospheric particles and scatter all wavelengths of visible light, producing the bright white of a typical cloud.
The Darkness of Clouds
Clouds that grow deep or tall enough look like gray clouds to an observer because less light is reaching their bases: The white tops and sides of the cloud scatter most of the sunlight, allowing less to pass through to the interior and bottom. Larger water droplets are more effective than smaller ones at absorbing rather than scattering sunlight, and can thus create a darker shade. A sheet of stratus clouds covering the sky – called opacus – also naturally blocks sunlight and takes on a gray cast.
It’s also possible for clouds to look dark simply because they’re in the shadow of a nearby cloud, or because the setting sun is only illuminating their tops. Your position as an observer in relation to the cloud and the sun matters in other ways, too: If you’re between the sun and a tall cumulus, the cloud appears a dazzling white, but on the other side you’ll see it as gray because of the blocked and scattered rays.
Dark Rain Clouds
As the above discussion suggests, a dark-bottomed cloud doesn’t necessarily mean an impending downpour, though those with a deep bruised gray or blackish underside certainly warrant attention. Nimbus clouds get their intimidating look from the scattering of sunlight at their upper reaches and margins, and the absorption of sunlight by large water droplets, Again, those larger droplets absorb more sunlight, so a darkening cloud may indicate one in which water droplets are getting heavy enough to begin falling. Dark storm clouds also cast shadows: The “anvil» of a full-grown cumulonimbus, for example, may shroud the cloud’s trailing edge.
One visual clue to distinguish between your garden-variety dark cloud that’s simply deep enough to limit sunlight transmission and an actual rain-bearing cloud is the latter’s fuzzy-looking base, created by falling precipitation. A big thunderhead may also show a fuzzy, if bright, crown, which is the result of water droplets turning to ice at the high altitude of the cloud top.
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Noun — Adjective — Verb — Related words and phrases
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ShumilinaElenaTeacher
Terms in this set (20)
Noun — Adjective — Verb — Related words and phrases
Сущ. — Прил. — Гл. — Родственные слова и фразы
cloud — cloudy — x — rain cluods, storm clouds
облако — облачно — x — дождевые тучи, грозовые тучи
fog — foggy — x — x
туман — туманно — x — x
frost — frosty — x — frostbite
мороз — морозный — х — обморожение
hail — x — to hail — hail storm
град — х — идти (о граде) — шторм с градом
ice — icy — x — x
лед — ледяной — x — x
lightning — x — x — flash of lightning
молния — x — x — вспышка молнии
mist — misty — x — x
легкий туман, дымка — туманный — x — x
rain — rainy — to rain — raindrop
дождь — дождливый — идти (о дожде) — капля дождя
shower — showery — x — rain shower
ливень — ливневый, проливной — x — проливной дождь
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‘DARK LOW CLOUD’ is a 12 letter
Phrase
starting and ending with D
Crossword answers for DARK LOW CLOUD
Synonyms for STRATUS
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