Prevention / relaxation control method for weather disaster

Abstract

To provide a feasible method for prevention / relaxation control over a weather disaster caused by wind and rain of a typhoon etc.SOLUTION: A prevention / relaxation control method for weather disaster includes stopping a typhoon and local heavy rain by dispersing energy of a flow of the atmosphere by the use of simple impact means at optimum timing in an optimum place before the typhoon and local heavy rain occurs so as to perform prevention / relaxation control over a weather disaster in an easily feasible manner.SELECTED DRAWING: Figure 6

Description

Technical Field

[0001] The present invention relates to a method for preventing and mitigating meteorological disasters caused by wind and rain such as typhoons.

Background Art

[0002] Measures against meteorological disasters caused by wind and rain such as typhoons have been an important issue not only in Japan but also around the world since ancient times, and measures centering on civil engineering works for flood control and water utilization have been carried out in various forms.

[0003] However, typhoons and concentrated heavy rains are becoming more frequent and powerful, and it is a reality that they are causing great damage to human society such as floods without effective countermeasures.

[0004] On the other hand, a method of using a powerful bomb to eliminate a typhoon is disclosed in, for example, Japanese Patent Application Laid-Open No. 2018-077204 (Patent Document 1), but it uses nuclear bombs and hydrogen bombs and is not at all feasible.

Prior Art Documents

Patent Documents

[0005]

Patent Document 1

Summary of the Invention

Problems to be Solved by the Invention

[0006] An object of the present invention is to provide a feasible method for preventing and mitigating meteorological disasters caused by wind and rain such as typhoons.

Means for Solving the Problems

[0007] The method for preventing and mitigating meteorological disasters, which was developed to solve the above problems, involves the generation of water vapor over the ocean near the equator, the generation of updrafts in which the water vapor rises, the generation of clouds due to the cooling of the rising water vapor, the growth of the clouds into cumulonimbus clouds, the gathering of a large number of cumulonimbus clouds to form a vortex and the development of a tropical depression as the atmospheric pressure near the center drops, and the development of the tropical depression into a typhoon with a wind speed exceeding 17 m / s. During the process of typhoon formation, inside the gathered cumulonimbus clouds and the tropical depression before they turn into a typhoon, an impact means is used to impart an impact to the atmosphere to disrupt the atmospheric flow and disperse the energy of the atmospheric flow. This is the characteristic feature.

[0008] According to the present invention described above, by dispersing energy using an impact means at an initial stage before a tropical depression grows into a typhoon, the occurrence of future typhoons can be avoided, and meteorological disasters caused by wind and rain can be prevented and mitigated.

[0009] Also, another method for preventing and mitigating meteorological disasters involves, in the cumulonimbus clouds in a temperate depression, in front of the confluence point of cumulus clouds from the west and cumulus clouds from the south containing a large amount of water vapor, inside the cumulus clouds and cumulonimbus clouds before heavy concentrated rainfall occurs, an impact means is used to impart an impact to the atmosphere to disrupt the atmospheric flow and disperse the energy of the atmospheric flow. This is the characteristic feature.

[0010] According to the above invention, by dispersing energy using an impact means inside the converging cumulus clouds and cumulonimbus clouds before heavy concentrated rainfall occurs, the occurrence of future heavy concentrated rainfall can be avoided, and meteorological disasters caused by wind and rain can be prevented and mitigated.

[0011] Furthermore, when the impact means is an explosive, the explosive consists of a first firework and a second firework, and the first firework and the second firework are successively dropped from above the cumulus clouds and cumulonimbus clouds and exploded simultaneously or with a time difference. By exploding two explosives at different altitudes, the energy can be effectively dispersed.

[0012] In addition, the first firework and the second firework each have a main body, a weight disposed on the bottom side of the main body, and a tail fin disposed on the top side of the main body. Inside the main body, a central explosion part and an outer peripheral explosion part disposed horizontally with respect to the central explosion part are arranged. When dropped, due to air resistance, the weight assumes a posture where it is downward and the tail fin is upward. When it explodes in this posture, a two-stage and wide-range explosion can occur, thereby more effectively dispersing energy, and it can explode in the correct posture without falling over.

[0013] When the impact means is the jet of a jet engine mounted on an aircraft, and the aircraft passes through the inside of the cumulus cloud, cumulonimbus cloud, tropical depression or temperate depression, the energy of the atmospheric flow can be dispersed more quickly and easily.

Advantages of the Invention

[0014] According to the present invention, by dispersing the energy of the atmospheric flow using simple impact means at the optimal timing and location before a typhoon or heavy rainstorm occurs, a typhoon or heavy rainstorm can be prevented, and thus a method for preventing and mitigating meteorological disasters that is easy to implement can be provided.

Brief Description of the Drawings

[0015]

Figure 1

Figure 2

Figure 3

Figure 4

Figure 5

Figure 6

Figure 7

Figure 8

Embodiment for Carrying Out the Invention

[0016] First, the inventor's idea regarding the mechanism of typhoon generation will be described with reference to FIGS. 1 and 2.

[0017] Typhoons are generally considered to be generated by the following four elements. 1. Starting with the spherical body drop of extensive cumulus clouds (rapid cooling in the upper atmosphere even near the equator) 2. With the fastest rotation speed at the equator, faster on the equator side, and extensive dropping while the spherical cumulus clouds horizontally rotate and accelerate 3. Affected by the high-pressure wall in the northern temperate zone and the atmospheric current, water vapor and moisture are involved and a huge vortex is formed 4. An updraft is generated at the escape opening of water vapor, moisture, and air in the central part, and a torsional updraft in the same direction as the overall rotation begins

[0018] That is, the seawater near the equator in the Northern Hemisphere is heated by the sun's heat and evaporates into water vapor. The water vapor that has concentrated in a certain place begins to rise while swirling counterclockwise due to rotation, generating an updraft. The rising water vapor is cooled by the cold air in the upper atmosphere and becomes water droplets to form clouds. When this water vapor becomes water droplets and clouds, a lot of heat is released into the atmosphere. This heat warms the surrounding air, strengthening the updraft, and humid air continuously flows in, and the clouds eventually grow into cumulonimbus clouds. Then, a number of cumulonimbus clouds gather to form a vortex. The air pressure near the center of the vortex drops, and it further develops into a tropical depression. When the wind speed exceeds 17 m / s, it is called a typhoon.

[0019] As described above, a "water vapor and moisture cycle" of central ascent, spreading to the surroundings at the top, and rapid cooling and dropping is formed. As long as there is water vapor and moisture to be sucked up, it proceeds (moves) under the influence of ocean currents and atmospheric currents.

[0020] Regarding the mechanisms of the Earth's rotation and revolution, gravity (gravitational force), a large amount of water vapor and moisture, temperature differences, physical actions, etc., there are various theories, and it can be said that it is a miraculous phenomenon with all the main elements.

[0021] Due to the increase in electromagnetic radio waves and electric currents, and the sharp increase in floating particulate dust, the circulation of water vapor depending on the original Earth environment is greatly hindered. The concentration saturation in the confluence of air currents and air masses in local areas becomes frequent and intensified, which is considered to be the cause of the frequent occurrence of abnormal low pressures. Therefore, it is considered that means to assist the elevation and diffusion of water vapor are necessary, and the present invention has been achieved.

[0022] This will be described based on Figure 3. The generated water vapor, clouds, etc. are in the environment during the launch and acceleration of vehicles, etc. At the equator, due to the difference in the Earth's rotation speed, for extensive cumulus clouds, the force on the equatorial side prevails and rotates (low pressure). For objects that are stable due to gravity such as atmospheric objects, the opposite force acts, so the high-pressure atmosphere rotates in the opposite direction. Although it is difficult to eliminate a developed typhoon, with the rapid progress of civilization and science, and the current availability of accurate information on typhoon occurrence, it is considered that the underdeveloped tornadoes and typhoons immediately before and after occurrence can surely be controlled.

[0023] As described above, it is considered that typhoons are generated when the four predetermined elements are present. Therefore, it was considered that by disrupting the mechanism before the four elements for typhoon generation are present, the future occurrence of typhoons can be prevented and moderately controlled.

[0024] That is, it is possible to disrupt the mechanism by dispersing energy while it is a tropical depression or during the small-scale stage immediately after the occurrence as a typhoon. Specifically, it was decided to use a method of dropping explosives from the outside and utilizing the energy of the explosion.

[0025] Moreover, this mechanism is not limited to typhoons. When the air currents converge immediately before the occurrence of tornadoes or concentrated heavy rain, it is also possible to prevent the occurrence of tornadoes, concentrated heavy rain, etc. by disturbing the air flow with impact means such as explosives and dispersing the energy of the air flow, and it can be realized without using special means that are difficult to achieve such as nuclear bombs.

[0026] The explosive has a structure similar to that of a fireworks rocket, and since multiple explosives are required, they are used in pairs of a first firework and a second firework. The first firework and the second firework are successively dropped from a dropping means above the tropical depression, and are exploded either simultaneously or with a time difference. Note that three or more fireworks may be used as the third firework, the fourth firework, and so on.

[0027] FIG. 4 is a view showing a first firework 100 which is an explosive used in a preferred embodiment of the present invention. The first firework 100 has a spherical main body 10, a weight 20 disposed on the bottom side of the main body 10, and a tail fin 30 disposed on the top side of the main body. Inside the main body, a central explosion part 40 and four outer peripheral explosion parts 50 arranged horizontally with respect to the central explosion part 40 are disposed. Since the second firework 200 has the same structure, a detailed description thereof will be omitted. The sizes of the first firework and the second firework may be the same or different.

[0028] In the present embodiment, the weight 20 may be disposed either inside or outside the main body. Although a spherical main body 10 is used, a bullet-shaped body having a hemispherical end and a cylindrical end may be used.

[0029] FIG. 5 is an explanatory view showing the dropping location of the explosive, and FIGS. 6 to 7 are views showing the state of explosion. As shown in these figures, the first firework and the second firework are successively dropped from an aircraft which is a dropping means to the center of the low pressure and exploded.

[0030] When the first firework 100 is dropped from an aircraft which is a dropping means, due to air resistance, the weight 20 assumes a posture where it is downward and the tail fin 30 is upward, and it explodes in that correct posture.

[0031] At the time of explosion, the central explosion part 40 ignited by the fuse 60 first explodes and diffuses the outer peripheral explosion parts in all directions, and the outer peripheral explosion parts 50 explode at positions away from the central explosion part 40.

[0032] In this way, by adopting a two-stage explosion with a structure similar to that of a fireworks rocket, the energy of the explosion can be transmitted over a wide range in the horizontal direction to diffuse the energy of the low pressure.

[0033] By causing the first firework 100 and the second firework 200 dropped continuously to explode with a difference in altitude, the energy of the explosion can be transmitted over a wide range in the vertical direction to disperse the energy of the low pressure.

[0034] The low pressure to be dropped is a tropical depression generated over the ocean near the equator, specifically, a tropical depression generated over the ocean near the equator from the Tropic of Cancer to the Tropic of Capricorn.

[0035] By dispersing the energy of the explosive in the initial stage before the low pressure moves to the Northern Hemisphere or the Southern Hemisphere and grows into a typhoon in this way, the occurrence of future typhoons can be avoided, and meteorological disasters caused by wind and rain can be alleviated and controlled.

[0036] Regarding the linear precipitation band, it is considered that the generation mechanism is the same as that of a typhoon, except that it does not rotate.

[0037] This will be described with reference to FIG. 8. Water vapor generated over the ocean rises by the updraft and advances (moves) under the influence of ocean currents and air currents. In Japan, it is considered to develop at the confluence point of the air current from the continent and a large amount of water vapor from the ocean and turn into a linear precipitation band.

[0038] Therefore, by dropping an explosive onto the confluence point of the fluid (cloud) of the tropical depression over the sea and causing an explosion, similar to a typhoon, mitigation and control of meteorological disasters can be achieved. The confluence point is predicted by scientific technology using meteorological satellites and the like.

[0039] In addition, it is also conceivable that the impact means is the injection of a jet engine mounted on a jet plane flying straight to the site, and the jet plane passes through the inside of the cumulus cloud, cumulonimbus cloud, the tropical depression, and the temperate depression to disperse the energy of the air flow. It is more effective if it is a dedicated disaster prevention jet plane that can fly straight to the destination quickly.

Explanation of Signs

[0040] 10 Body, 20 Hammer, 30 Tail fin, 40 Central explosion part, 50 Outer peripheral explosion part, 60 Fuse, 100 First firework, 200 Second firework

Claims

1. In the process of typhoon formation, where water vapor is generated over the ocean near the equator, an updraft in which the water vapor rises is generated, clouds are formed by cooling the rising water vapor, the clouds grow into cumulonimbus clouds, a large number of cumulonimbus clouds gather to form a vortex and the atmospheric pressure near the center drops to develop into a tropical depression, and the tropical depression develops into a typhoon with a wind speed exceeding 17 m / s, inside the gathered cumulonimbus clouds and the tropical depression before it becomes a typhoon, an impact means is used to impact the atmosphere to disrupt the air flow and disperse the energy of the air flow. A method for preventing and mitigating meteorological disasters, characterized by this.

2. In the cumulonimbus clouds in an extratropical depression, before the confluence point of cumulus clouds from the west and cumulus clouds from the south containing a large amount of water vapor, inside the cumulus and cumulonimbus clouds before heavy concentrated rainfall occurs, an impact means is used to impact the atmosphere to disrupt the air flow and disperse the energy of the air flow. A method for preventing and mitigating meteorological disasters, characterized by this.

3. The impact means is an explosive, and the explosive consists of a first firework and a second firework. The first firework and the second firework are successively dropped from above the cumulus clouds and (or) the cumulonimbus clouds and exploded simultaneously or with a time difference. The method for preventing and mitigating meteorological disasters according to claim 1 or 2, characterized by this.

4. The first firework and the second firework have a main body, a weight arranged on the bottom side of the main body, and a tail fin arranged on the top side of the main body. Inside the main body, a central explosion part and an outer peripheral explosion part arranged horizontally with respect to the central explosion part are arranged. When dropped, due to air resistance, the weight takes a posture where it is downward and the tail fin is upward, and it explodes in that posture. The method for preventing and mitigating meteorological disasters according to claim 3, characterized by this.

5. The impact means is the injection of a jet engine mounted on a jet aircraft, and the jet aircraft passes through the inside of the cumulus clouds, cumulonimbus clouds, the tropical depression, and the extratropical depression to disperse the energy of the air flow. The method for preventing and mitigating meteorological disasters according to claim 1 or 2, characterized by this.

Images