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Thunder-carrying clouds are regional.
It is not difficult to find that 1. The movement of clouds is not divided into fast and slow (friction conditions), and the cloud system from the direction of the ocean generally does not produce thunder and lightning, and the obvious characteristics are; The raindrops are small and dense, the rainfall is long, and the sky is relatively quiet. 2. Under similar weather conditions, the cloud system in the southeast and northeast directions occasionally has several lightning activities, and most of them belong to the spiral cloud system (the cloud generation area is unknown), which is characterized by; The raindrops are large, the wind direction is uncertain, and the rain is violent and short-lived. 3. In the sultry weather, the cloud system from the northwest direction is mostly stormy, lightning and thunder, and the rainfall time is short, and there are more when the rain is clear.
As the saying goes: look at the southeast in the morning and the northwest in the evening, the cloud system of rain and thunder and lightning does have directionality, and it is difficult to change the laws of nature, and what needs to be changed is people's cognition and discovery.
The energy of thunder and lightning in the clouds is provided by the earth's surface, and the components that provide this energy are electrostatic electrons, and water vapor is its carrier. This is the explanation of the formation of thunder and lightning in "Exploring the Field of Physics", and at present, students all over the world are being educated; "Under the influence of strong convective weather, the friction between the clouds produces thunder and lightning. The only correct answer to the two theories depends on the laws of nature, so please pay attention to this topic.
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All contain thunder and lightning.
Clouds collide with each other in the sky, generating high-voltage static electricity, which is then discharged to the nearest part of the ground, creating thunder and lightning.
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In the thunderstorm season, most of the cloud systems carrying thunder and lightning in most parts of China come from the northwest, southeast, northeast and easterly cloud systems. Less lightning activity (with the exception of spiral clouds). It is not difficult to see that the northwesterly clouds come from the inland, and the southeast, northeast, and easterly clouds come from the ocean. In this regard, we analyze the following aspects of natural phenomena.
The textbook says: "Due to the influence of strong convective weather, the friction between the clouds produces thunder and lightning." "1. The cloud system in the northwest direction is prone to storms, lightning and thunder and even hail disasters, and the rainfall time is short, and most of them are sunny after rain.
2. The raindrops in the cloud system in the direction of the ocean are small, the rainfall time is long, and the sky is relatively quiet, this kind of weather is more common, and the typhoons are generated in the ocean, and the number of typhoons is relatively less after landfall. 3. There is no detailed explanation of seasonality in the book, and snowstorms are also a form of severe convective weather, but there is no thunder and lightning activity.
The textbook also says: "The air expands and rises when it is heated, and cold air from elsewhere comes to replenish it, so that the wind is formed." "People often hear this term to describe the weather when cold air moves south and warm and humid air flows north, but the reason for this is more complicated when cold clouds and clouds are prone to thunder and lightning and few people observe them.
There are all kinds of indications that water molecules are substances with a very small coefficient of friction, and even have a lubricating effect, and even if friction occurs, it will not produce electricity! This is a serious way to explain nature, because what is said in textbooks is a definition or a theory, and students all over the world are learning about it.......
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Thunderstorm clouds are a mature thunderstorm cloud that can stretch up to a height of 40 (about 10,000 meters or more) at the top, while the temperature at the base of the cloud is above 10. Because the clouds cross such a wide range of temperatures vertically, the phases of the water vapor consolidates in the clouds are very different. There are water droplets, supercooled water droplets, snow crystals, ice crystals, etc. in the clouds (see Figure 2).
If we stratify thunderstorm clouds according to their temperature, we can see that in the "warm layer" clouds with a temperature higher than 0, all are water droplets (including cloud droplets), and in the clouds with a temperature of 0 to 8, there are more supercooled water droplets (water droplets with a temperature lower than 0), and there are also some snow crystals and ice crystals; In clouds with temperatures below 20, the natural icing nucleation of ice crystals in the clouds is more significant due to the increased probability of natural freezing of supercooled water droplets, so the clouds are basically full of snow crystals and ice crystals. In the mature stage of thunderclouds, very complex microphysical processes take place, in the "warm layer" of the clouds, there are gravitational collisions between water droplets due to different sizes, turbulent collisions, and electrical and acoustic collisions.
At the same time, there are large water droplets that deform under the action of air flow and break to produce a "chain reaction"; There are also large snowflakes and graupel that fall from the "cold layer" of clouds to the "warm layer". In clouds with a temperature of 0 to 20, water vapor is very active in the transfer from liquid to solid, and the adhesion of ice and snow crystals, and the breakage of large ice crystals are also frequent. In clouds below 20, there is also the process of adhesion between ice crystals and the fragmentation of large ice crystals.
All these microphysical processes that occur in thunderstorm clouds can lead to changes in the electrical state of water vapor condensates in the clouds, which contribute very much to the electrification of thunderstorm clouds.
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It is due to the fact that the charges on two clouds that are close to each other are different, one is positive and the other is negative, and when the two clouds reach a certain distance, the discharge phenomenon will occur, and then thunder and lightning will be generated.
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Lightning is a phenomenon of electrical discharge, but it is not confined to clouds.
Due to the fact that the wind speed and direction are not exactly the same at different altitudes, the water droplets and ice crystals between the clouds rub against each other to produce static electricity. Voltage accumulation can reach tens to millions of volts, causing the air to ionize and discharge.
The clouds dotted the ground to induce electricity, and the man in the wilderness acted as a tip protrusion on the surface of a sleek conductor. Since the earth conducts electricity, it must objectively be an equipotential body, so that the human body is charged in large quantities and is more prone to ionization.
This answer is not very exhaustive and requires a high school electrical foundation, please let me know via PM for questions or other insights.
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Ionization... Then there will be charged clouds, and the opposite of the clouds will form a discharge.
It's not that general.
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Lightning is a large-scale electrical discharge phenomenon that occurs in the sky. Clouds in the sky, some positively charged and some negatively charged; Large-scale discharges occur when two clouds with different types of electricity are close to each other. The electric spark that appears when discharging is lightning, and the sound it makes is thunder.
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