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THE SPIRITUAL SUN There has been much published on HAARP and its purposes. There is no way a small group of people can be effective against HAARP, nor is. Joanne Nova and Anthony Cox. The theory that failed. It takes only one experiment to disprove a theory. The climate models are predicting a global disaster, but the. Intellicast.com: The Authority in Expert Weather. Universal Time: Tuesday,, 02:36.
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Latest trending topics being covered on ZDNet including Reviews, Tech Industry, Security, Hardware, Apple, and Windows. The sky is that beautiful old parchment in which the sun and the moon keep their diary.
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Cloud - Wikipedia. In meteorology, a cloud is an aerosol comprising a visible mass of minute liquiddroplets or frozen crystals, both of which are made of water or various chemicals. The droplets or particles are suspended in the atmosphere above the surface of a planetary body.
The air may be cooled to its dew point by a variety of atmospheric processes or it may gain moisture (usually in the form of water vapor) from an adjacent source. Nephology is the science of clouds which is undertaken in the cloud physics branch of meteorology. Cloud types in the troposphere, the atmospheric layer closest to Earth's surface, have Latin names due to the universal adaptation of Luke Howard's nomenclature. It was formally proposed in December 1.
It became the basis of a modern international system that classifies these tropospheric aerosols into five physical forms and three altitude levels or . These physical types, in approximate ascending order of convective activity, include stratiform sheets, cirriform wisps and patches, stratocumuliform layers (mainly structured as rolls, ripples, and patches), cumuliform heaps and tufts, and very large cumulonimbiform heaps that often show complex structure. The physical forms are cross- classified by altitude levels to produce ten basic genus- types or genera. Some of these basic types are common to more than one form or more than one . Most genera can be divided into species, some of which are common to more than one genus.
As the Sun burns hydrogen at its core, it releases vast amounts of atomic particles, or pieces of atoms, into outer space. These atomic particles along. COSMIC DUST CLOUD - INCOMING. YOU'VE BEEN WARNED BEFORE!!! 3 INCOMING MONSTERS largest one in November. Cloud Reading Divination. Article by Craig Hamilton-Parker. As a child, did you ever lie on your back in the garden and watch cumulus clouds to see what pictures you.
These can be subdivided into varieties, some of which are common to more than one genus or species. Cirriform clouds that form higher up in the stratosphere and mesosphere have common names for their main types, but are sub- classified alpha- numerically rather than with the elaborate system of Latin names given to cloud types in the troposphere. They are relatively uncommon and are mostly seen in the polar regions of Earth. Clouds have been observed in the atmospheres of other planets and moons in the Solar System and beyond.
However, due to their different temperature characteristics, they are often composed of other substances such as methane, ammonia, and sulfuric acid as well as water. Classification of major types.
While the link between cosmic rays and cloud cover is yet to be confirmed, more importantly, there has been no correlation between cosmic rays and global temperatures. BREXIT RISK RISING — Time to stop ignoring Brexit. Multiple polls now show U.K.
Stratiform. Cirriform. Stratocumuliform. Cumuliform. Cumulonimbiform. Extreme level. Noctilucent. Very high level. Nacreous.
High- level. Cirrostratus. Cirrus. Layered Cirrocumulus. Tufted Cirrocumulus. Mid- level. Altostratus.
Layered Altocumulus. Tufted Altocumulus. Low- level. Stratus. Stratocumulus. Small Cumulus. Multi- level/vertical. Nimbostratus. Moderate Cumulus.
Towering vertical. Towering Cumulus. Cumulonimbus. Etymology. Around the beginning of the 1. Over time, the metaphoric term replaced the original old English weolcan to refer to clouds in general.
In about 3. 40 BC the Greek philosopher Aristotle wrote Meteorologica, a work which represented the sum of knowledge of the time about natural science, including weather and climate. For the first time, precipitation and the clouds from which precipitation fell were called meteors, which originate from the Greek word meteoros, meaning 'high in the sky'. From that word came the modern term meteorology, the study of clouds and weather. Meteorologica was based on intuition and simple observation, but not on what is now considered the scientific method. Nevertheless, it was the first known work that attempted to treat a broad range of meteorological topics.
Rain is produced from the compression of a closely condensed cloud, varying according to the pressure exerted on the cloud; when the pressure is slight it scatters gentle drops; when it is great it produces a more violent fall, and we call this a shower, being heavier than ordinary rain, and forming continuous masses of water falling over earth. Snow is produced by the breaking up of condensed clouds, the cleavage taking place before the change into water; it is the process of cleavage which causes its resemblance to foam and its intense whiteness, while the cause of its coldness is the congelation of the moisture in it before it is dispersed or rarefied. When snow is violent and falls heavily we call it a blizzard. Hail is produced when snow becomes densified and acquires impetus for a swifter fall from its close mass; the weight becomes greater and the fall more violent in proportion to the size of the broken fragments of cloud. Such then are the phenomena which occur as the result of moist exhalation. Several years after Aristotle's book, his pupil Theophrastus put together a book on weather forecasting called The Book of Signs. Various indicators such as solar and lunar halos formed by high clouds were presented as ways to forecast the weather.
The combined works of Aristotle and Theophrastus had such authority they became the main influence in the study of clouds, weather and weather forecasting for nearly 2. Howard was a methodical observer with a strong grounding in the Latin language and used his background to classify the various tropospheric cloud types during 1. He believed that the changing cloud forms in the sky could unlock the key to weather forecasting. Lamarck had worked independently on cloud classification the same year and had come up with a different naming scheme that failed to make an impression even in his home country of France because it used unusual French names for cloud types.
His system of nomenclature included twelve categories of clouds, with such names as (translated from French) hazy clouds, dappled clouds and broom- like clouds. By contrast, Howard used universally accepted Latin, which caught on quickly after it was published in 1.
An elaboration of Howard's system was eventually formally adopted by the International Meteorological Conference in 1. Cumuliform clouds forming in the lower level were given the genus name cumulus from the Latin word for heap. Physically similar clouds forming in the upper . Cirriform clouds were identified as always upper level and given the genus name cirrus from the Latin for 'fibre' or 'hair'.
In addition to these individual cloud types; Howard added two names to designate cloud systems consisting of more than one form joined together or located in very close proximity. Cumulostratus described large cumulus clouds blended with stratiform layers in the lower or upper levels. Altocumulus floccus producing virga near top and middle of image merging into altostratus translucidus near horizon. During the mid 1. Emilien Renou, director of the Parc Saint- Maur and Montsouris observatories, began work on an elaboration of Howard's classifications that would lead to the introduction during the 1. These were respectively stratocumuliform and stratiform cloud genera of a newly defined middle .
However, he also proposed and had accepted by the permanent committee of the International Meteorological Organization (IMO), a forerunner of the present- day World Meteorological Organization (WMO), the designation of a new free- convective vertical or multi- . With this addition, a canon of ten tropospheric cloud genera was established that came to be officially and universally accepted.
He proposed the name noctilucent which is Latin for night shining. Because of the extremely high altitudes of these clouds in what is now known to be the mesosphere, they could become illuminated by the a sun's rays when the sky was nearly dark after sunset and before sunrise. The latter had become the first researcher to use photography for the study and classification of clouds in 1.
Heinrich Dove of Germany and Elias Loomis of the United States came up with other schemes in 1. Clayton (1. 89. 6), but their systems, like earlier alternative schemes, differed too much from Howard's to have any success beyond the adoption of some secondary cloud types. It was then renamed nimbostratus and published with the new name in the 1.
International Atlas of Clouds and of States of the Sky. During its 7. 8- day mission, it relayed thousands of pictures showing the structure of large- scale cloud regimes, and proved that satellites could provide useful surveillance of global weather conditions from space. It was co- sponsored by NASA and showed a change in name of the nimbiform type to cumulonimbiform.
These forms are commonly used for the purpose of satellite analysis. The stratiform group is divided by altitude range into the genera cirrostratus (high- . They form at high tropospheric altitudes in air that is mostly stable with little or no convective activity, although denser patches may occasionally show buildups caused by limited high- level convection where the air is partly unstable. They generally form as a result of limited convection in an otherwise mostly stable airmass topped by an inversion layer. The stratocumuliform group is divided into layered cirrocumulus (high- . In general, small cumuliform clouds tend to indicate comparatively weak instability.
Larger cumuliform types are a sign of moderate to strong atmospheric instability and convective activity. Tufted altocumulus and cirrocumulus genera in the middle and high . They occur in highly unstable air. Clouds with significant vertical extent occupy more than one . Stratocumuliform and stratiform clouds in the high .
When comparatively low- resolution satellite images of high clouds are analized without supporting data from direct human observations, it becomes impossible to distinguish between individual genus types which are then collectively identified as cirrus- type. They often form along a high altitude jetstream. It is composed of ice crystals or supercooled water droplets appearing as small unshaded round masses or flakes in groups or lines with ripples like sand on a beach. The sun and moon are visible in clear outline.
These clouds can form as low as 2,0. Without the addition of human observations, these clouds are usually collectively identified as 'middle- type' on satellite images.