What is the cloud cumulonimbus?
Cloud cumulonimbus is one of the largest clouds created in the weather samples. A high appearance similar to a column, often with a flat peak, may indicate a serious flash, heavy rain and high winds. Storm clouds are formed from rising warm air, which cools and creates ice at higher altitudes or height above the ground and rain at lower levels. They can also create hail and tornadoes that can cause damage to the crop and property and injury to humans and animals. If enough moisture or water vapor is present, clouds can be formed. The formation of kumulonimbus begins with smaller cumulus clouds that do not indicate serious weather. If the rising air is still pushing up, the cumulus clouds can rise to the towering cumulus, with tens of thousands of feet or meters. The formation of a drop of rain releases heat and can be created enough energy to create an increasing cloud.
When lightning starts, the kumulonimbus cloud has developed and now a storm is present. TVOba storms may appear as the only cloud formation, often called the storm of air or isolated cell. They can also be sorted along the front limit, which is a edge between the warmer, humid air mass and the colder dry air system. These storm lines are often called Squall Line thunderstorms and can create strong weather.
Clouds are constantly changing and cloud cumulonimbus is no exception. They pass through a life cycle, each phase having brands or properties. These phases are generally known as development, mature and scattered.
developing cloud Kumulonimbus absorbs heat from rising air, with rain and ice at various altitudes. As rain droplets release more heat, updrafts of rapid air can form in the cloud system. If sufficient moisture is transmitted and only the two or the sticks accumulate, hail can be formed.
Mature clouds kumulonimbus are usually called thunderstorms. The flash occurs when electricity is made from friction of water in the cloud. The forming cloud -like columns are formed with a flat top shape, often called anvil. The anvil is caused by when high -speed air, called current of the current, pushes the upper part of the storm in front of the column.
Mature storm can produce high winds of donut cold air and leave the bottom of the cloud known as microbursts or queues of defeat. Strong rain and frequent flash indicate that a ripe storm is taking place. Health can often be seen in the areas on the front of the storm, because the collected ice crystals are too heavy and fall in front of the storm.
Some weather conditions can create storms that are more dangerous. Super cell storm is a mature cloudbus cloud with internal rotation called mesocyclone. The air moves in different directions at different altitudes that the super cell rotates, which can cause tornadoes or serious winds.Super cells can be very stable systems and dangerous weather can occur over long distances for a long time.
As the storm continues, the rain falls over the cloud, removes moisture and changes the flow of air. The heat that caused a rapid updraft air in the developing storm is gone and the storm begins to distract, with some areas of rain, but less wind. The structure of the cloud rods begins to crumble and the cloud cumulonimbus becomes either a more uniform layer of clouds or disappears.
other types of clouds can show that the storm is coming. Cirus clouds are very thin layers of ice crystals in high altitudes, often called miserable or feathers. In fact, these ice crystals are the peaks of Cumulonimbus clouds at a certain distance that have been shifted forward winds with a high altitude, called a current of the current. Cirrus clouds may be a sign that the stormy weather is a day or two away because the stream moves faster than the storm area.