Jacques Cousteau cloud, or also can be called undulatus asperatus. The official name undulatus clou

Polar stratospheric clouds form in the stratosphere at an altitude of 50,000 box making to 80,000 feet. These clouds are classified into Type I (clouds form more diffuse and less bright colors). Unfortunately, Polar stratospheric clouds play a key role in the massive ozone depletion over the Arctic and Antarctic. NASA explains that this cloud is formed box making only at very low temperatures. In recent years, the atmosphere over the Arctic colder box making than usual, and this polar stratospheric clouds continued until the spring. As a result, ozone levels continue to decline.
Jacques Cousteau cloud, or also can be called undulatus asperatus. The official name undulatus clouds asperatus taken because the undulation shape can be described as a cloud of highly turbulent and chaotic. According to Guardian.co.uk, box making the Roman poet Virgil asperatus use the word in a poem to describe the wavy sea surface due to the north wind.
Noctilucent clouds appeared several times in Europe and the United States. Scientists believe that they arise because box making it is caused by global warming. Because this phenomenon is basically new, apparently more questions than answers to this cloud phenomenon. Type of cloud was first observed 126 years ago by an amateur astronomer. Located in the mesosphere layer, noctilucent clouds are the highest clouds in the world. Clouds box making that form 50 miles above Earth's surface are generally colorless, although there are some pale blue, dark green, light yellow and sometimes red.
Anvil clouds are also known as cumulonimbus incus, consisting mostly of ice particles. This cloud is a storm cloud that has matured that a time may cause a storm and then a tornado. Cumulonimbus clouds are divided into two species: calvus and capillatus. There are enough interesting facts from the clouds, where the anvil clouds that are at the highest levels often contain heavy snow due to the very cold upper layer. The snow then melts into rain when it falls into a layer of warm air in the lowlands. According box making WeatherQuestions.com, 40 to 50% of the rain that is produced by the average box making storm originated as ice and snow, even for storms that occur in the tropics.
These clouds are usually formed due to gravitational waves. Stationary clouds can be classified into cirrocumulus standing lenticular (CCSL), altocumulus standing lenticularis (ACSL) and stratocumulus standing lenticular (SCSL). Because of its amazing forms, lenticular clouds are often mistaken mistaken for a UFO.
Morning Glory cloud is a rare phenomenon and dramatic. The cloud rolls occurs in the lower layers of the atmosphere ahead of the storm and can most often be observed in Northern Australia. Morning Glory clouds also been found in Germany, Central America, the English Channel and the East of Russia. This cloud length can reach up to 1000 km and sometimes there are up to seven or eight clouds are lined in a row. Despite being studied for over 70 years by scientists, remarkable atmospheric phenomena can not be clearly understood.
Mammatus cloud is a cloud formation that looks odd. Also known as mammatocumulus, they are often associated with the occurrence of severe storms. These clouds are formed due to convection and the buoyancy of the air. evaporation causes pockets of negative buoyancy so that the cold air trapped in the cloud. This makes the clouds puff downward instead of up like cumulus clouds, and they end up being like a reverse bubble.
Shelf cloud is like a shelf protruding from their parent thunderstorm clouds. This cloud formation associated with the phenomenon known as the "gust front". This type of cloud is often mistakenly thought to be a wall cloud. The difference is that clouds usually appear on the back wall of the storm, box making while Cloud Shelf in the front edge of the storm.
Cirrus radiatus clouds can be found in a variety of shapes and sizes and occur in the coldest and highest regions of the troposphere. Cirrus clouds are delicate and thin radiatus appear to converge to a single point on the horizon. The funny thing is that they only become parallel to each other and cirrus radiatus clouds were never united at all.
Kelvin-Helmholtz wave clouds look like ocean waves were crashing. This beautiful cloud named after its discoverer, namely two German box making physicist Hermann von Helmholtz and called his friend who is also a British physicist Lord Kelvin. These clouds are formed when two different layers of air moving past each other at different speeds. These clouds are often used as indicators for atmospheric instability.
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