10 sentences about clouds in english
Stratocumulus clouds are low puffy and grey. It is a slow-going process — each new piece of information must be incorporated throughout. Essay 3. Because the heating of the ocean and atmosphere is not uniform over the Earth, circulations are caused in both that transport heat and water — in particular, heat is transported by both the ocean and atmosphere away from the equator and towards the poles. There are not many types of mid-level clouds because most of them are not discovered. Essay 2. If all of the cloud water in the atmosphere were placed on the surface, the layer depth would only be 0. These are ways air can cool enough to form clouds: when air close to the ground is heated by the sun and rises to where the air is colder.
Cloud over the ocean, for instance, are different in some ways from clouds over land. Rossows, to gather better information about clouds and their radiative effects. Sometimes, clouds appear to be brilliant colors at sunrise or sunset. Another idea is that higher atmospheric temperatures could create denser clouds, since greater evaporation rates at higher temperatures would make more water vapour available in the atmosphere for cloud condensation.
Changing clouds can alter this relation, either increasing or decreasing the magnitude of the resulting temperature increase. Meteorologists have long associated greater cloud cover, higher cloud tops and denser, more reflective clouds with regions of more vigorous storms.
Over land there are more clouds, with higher reflectivity, in the afternoon. Clouds are made up of tiny water droplets or ice crystals.
Posted by. Nimbostratus clouds form a dark grey, wet looking cloudy layer associated with continuously falling rain or snow. Low, dense sheets of stratocumulus clouds hanging just above the ocean cool more than they heat.
Clouds for kids
Altostratus clouds are grey or blue grey mid-level clouds that are composed of ice crystals and water droplets. To understand clouds better, scientists are investigating the detailed behaviour of many different cloud types as defined by surface weather observers and cloud types as defined by weather satellites. Cumulus clouds are white, puffy clouds that look like pieces of floating cotton candy. Another 50 m of water is currently stored in the major ice sheets in Greenland and Antarctica. The question is — How many and which ones will actually take place when the climate changes and exactly how large will they be? Rossows, to gather better information about clouds and their radiative effects. Clouds form when the atmosphere can no longer hold all the invisible air vapor. Moisture condenses into fog when air is cooled from below. Worksheet Pack Moreover, changes in any of these climatic features may also affect the distribution and properties of clouds, but the understanding of clouds is so rudimentary that no one knows whether climate feedbacks involving clouds will dampen or amplify a warming trend. Most form in rows with blue sky visible between them. The early studies did not account for this possibility. This warming is partly reduced by other pollutants that form tiny aerosol particles which reflect some sunlight back to space. At some places in the tropics the western Pacific Ocean, the Amazon River Basin and the Congo River Basin , cloud tops extend up to 15 kilometers 50, feet , occasionally higher. Clouds are amazing, beautiful and interesting to us.
None of these energy and water exchanges can be understood without consideration of the effects of clouds on them, so quantitative cloud data, complemented by precipitation, water vapour, and radiative flux data, are required to diagnose these exchanges and their space-time variations.
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