WO2022083840A1 - Device for exerting an active effect on hydrometeorological processes - Google Patents

Abstract

The invention is directed toward allowing the assessment of actual and predicted meteorological data in a given region and the development and implementation of programs for exerting an active effect on atmospheric processes in order to reduce the negative consequences of weather factors in the interests of the national economy. This technical result is achieved in that the claimed device consists of component elements and units that are structurally combined to form a software/hardware system and are functionally combined by mathematical software for processing data, developing knowledge-based solutions and forming operating modes using artificial intelligence. A method for correcting atmospheric processes includes exerting an active effect on a region of maximum concentration of electrons in the ionospheric layer at a height of 90-120 kilometers using the claimed device, creating and developing vari-directional plasmic turbulence, and altering the pressure-temperature gradients in atmospheric processes, wherein an efficient effect is achieved by the resonant matching of the frequencies of an excitation wave and the natural oscillation frequencies of the plasma in the sporadic layer and by non-linear electromagnetic radiation effects in the ionosphere brought about by radiation generated in a unit for generating pulses using electroacoustic and polarized quasi-permanent electric fields.

Description

DEVICE FOR ACTIVE INFLUENCE ON HYDROMETEOROLOGICAL PROCESSES

Description of the invention

The present invention relates to the field of atmospheric physics, and specifically to applied meteorology and aeronomy.

The tasks of changing the weather, in order to correct precipitation, increase water resources and mitigate severe weather, mankind has tried to solve at all stages of its development. Modern action technologies began to develop after the discovery in the late 1940s of the fact that supercooled cloud droplets could be turned into ice crystals by introducing a reagent such as dry ice or artificial ice cores such as silver iodide. Research over the past 40 years has made it possible to better understand the microphysical processes of cloud evolution, the mechanisms of precipitation formation (rain, hail, snow), as well as the means and methods for their modification. However, bringing about deliberate and effective change through cloud seeding has always been more of a scientific and applied challenge than a well-established practice. Several dozen countries are currently implementing hundreds of remediation projects, particularly in arid and semi-arid regions of the world, where water scarcity prevents food and energy needs from being met and fire hazards are high.

1. From the prior art and methods of controlling atmospheric processes, two main directions in the development of technologies for active influences are known. Cloud seeding with

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SUBSTITUTE SHEET (RULE 26) reagents (dry ice, iodide compounds of silver, lead, calcium chloride, fine cement patent RU2138945 C1 dated 08/26/1998, and coarsely dispersed hygroscopic cement patent RU 2436289 C2 dated 12/20/2011) sold using aviation equipment and special-purpose ammunition . The second direction is the use of electrophysical methods implemented using ground-based devices, aerospace, and special ammunition.

Patent RU 2 694 200 C1 dated 07/09/2009 for a method of destroying the air temperature inversion layer in the troposphere by creating turbulence and an upward flow of air using plasma-optical ammunition as sources of turbulence and heat release with the help of rapid-fire artillery systems in order to artificially increase precipitation and improve weather conditions .

Patent RU2 462 026 C1 dated September 27, 2012 for a method of creating an upward flow of air in the atmosphere by heating it and enriching it with negative ions from grounded electrodes corona in the Earth's electric field and a multi-tiered system of tethered balloons with blackened balloons.

There are also combined methods of active influences, Patent RU 2 595 015 dated 20.08. 2016 (method of impact) on the atmosphere using a corona discharge, characterized in that in the process of generating a corona discharge, sulfuric acid vapor is added to the volume of the passing air flow.

However, all of the above methods assume the presence of cloud systems, water vapor and airborne condensation nuclei in the regions of work performed. Under adverse conditions, namely they are. the main threat of the formation of natural hazards, including agriculture,

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SUBSTITUTE SHEET (RULE 26) The claimed technologies are not very effective. It is known that the energy contained in natural meteorological systems is so great that it is impossible to create water vapor and artificial cloud systems that could produce rain. Creation of active impact technologies, which allow using disturbances that are weak relative to the energies of natural meteorological systems, but resonant in relation to them, make it possible to significantly change the natural course of the atmospheric process.

There is a known method of influencing charged airborne dispersions in order to modify weather conditions, described in patent RU 2 678 782 Cl A01G 15/00, 2017.12. a wave with an angular momentum in the absorption band of a charged airborne dispersion of a cloud emitted by an antenna with a variable radiation pattern and an electric field strength at the maximum of the antenna radiation pattern of at least 10 mV/m. The process of influencing the cloud is preceded by determining the speed and direction of movement of the airborne dispersion relative to the service area. The physical effect is achieved due to the transition of the angular momentum of the spiral wave to the external angular momentum of particles of a charged airborne dispersion, which has an electric dipole moment, as a result of which the neutral component of the dispersion is involved in the movement. The impact on the cloud is carried out by an electromagnetic wave for at least a minute.

This method can be effectively used in the presence of formed cloud systems and steam in the atmosphere, in order to

SUBSTITUTE SHEET (RULE 26) regulation of atmospheric precipitation in a normal synoptic situation and does not provide for the possibility of performing work in arid regions with high atmospheric pressure.

The device and method for igniting cosmic particles of an artificially ionized plasma structure in the atmosphere, set forth in US20070238252A1, 2005.09.06, describes local heating of the troposphere, which can generate acoustic atmospheric waves or gravity waves to modify steering winds that affect weather phenomena. Its implementation consists in irradiating the plasma with electromagnetic radiation emitted by antennas, which has a frequency higher than the electromagnetic radiation used to create a plasma layer to transfer energy to the air region at or near the plasma directivity as a means of thermodynamic heating of the air. Such a technique can be used to generate areas of heated air and to generate acoustic waves and gravity waves in the atmosphere for weather modification purposes. Such an impact involves only the acceleration of cloud systems, it is known that by heating the air, the moisture leaves saturation and the clouds dissipate, for the formation of clouds it is necessary either to introduce additional moisture during evaporation, or to cool the air in the layer.

This invention has been successfully used for research purposes on the interaction of electromagnetic radiation with the ionosphere. However, technologies for using high-power radiation to create a plasma layer and the possibility of transferring energy for dynamic air heating are highly costly and unsafe due to the lack of control over the energy efficiency of an artificially created plasma lens over the emitters. At

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SUBSTITUTE SHEET (RULE 26) At the same time, to correct weather conditions in a given region, this invention does not provide for additional devices and methods of directed action.

The closest analogues to the declared from the field of technology have not been identified. The tasks solved by the present invention for the correction of atmospheric processes, and in particular an increase or decrease in the amount of precipitation in a given area, are achieved by using modulated electromagnetic radiation interacting with various ionized phases of the layers E, F and adjacent perturbed layers of natural plasma turbulences, carried out in resonance with their own oscillations of ionized phases.

Resonantly induced changes in the position of the most ionized layer in the thermosphere and the corresponding process of thermodynamic perturbation transfer from the ionosphere to the earth's surface cause local changes in dynamic processes in the Earth's atmosphere with a radius of up to 300 kilometers in the horizontal plane and to the height of the troposphere - in the vertical plane, followed by a change in meteorological parameters such as pressure and temperature, which makes it possible to predictably build strategies for correcting weather conditions in the impact zone.

The technical result achieved by using the proposed invention is the possibility of assessing the actual and forecast data of weather conditions in a given region, developing and implementing programs for actively influencing atmospheric processes in order to reduce the negative effects of weather factors in the interests of the national economy.

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SUBSTITUTE SHEET (RULE 26) The technical result is achieved by the fact that the device for actively influencing hydrometeorological processes using combined electromagnetic radiation consists of constituent elements and blocks structurally integrated into a software and hardware complex that includes a block for analyzing actual data and physical predictors of meteorological and heliogeocosmic parameters, a block for generating executive modes of operation and controlling a combined generator electromagnetic radiation of the optical and radio frequency spectrum, a block of emitters of low-intensity electromagnetic pulses modulated by acoustic and polarized quasi-constant electric fields, focused near the vertical direction to the turbulent layers of the lower ionosphere, functionally integrated by software and mathematical software for data processing, development of expert solutions and formation of operating modes based on artificial intelligence . The analysis unit includes a digital meteorological station and a recorder of electric and magnetic radiation levels designed to assess changes in physical parameters in the surface layer and a database of space weather parameters obtained from open Internet sources, monitoring the effectiveness of those performed, which allows for active influence and adjustment of executive programs in real time. The expert system is implemented on the basis of intellectual and statistical analysis of the received data, automatically detects signs and microphysical characteristics, which

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SUBSTITUTE SHEET (RULE 26) allows, under the influence of resonant radiation, to correct the natural course of the atmospheric process. The result of data analysis and processing is an executive program of operating modes, including: the start time and duration of exposure, the choice of the number of emitters involved, the modulation mode of the emitter signals in frequency and amplitude, determining the azimuth and focus angle of the emitter block. When choosing the location of the elements and blocks of the complex and the modes of active impact, the parameters of geodetic, geological, environmental and hydrometeorological engineering surveys are analyzed, which ensures the elimination of the influence of negative technogenic and geopathic factors on the efficiency of the work performed.

The tasks to be solved using the invention make it possible to reduce the negative impact of weather factors on human life in a given region, and can be used in the interests of agriculture, fire protection measures, and emergency response. A method for correcting atmospheric processes, including active influence on the region of maximum electron concentration of the ionospheric layer with a height of 90-120 kilometers using the device of claim 1, the creation and development of plasma turbulence of different directions, the change in thermobaric gradients in atmospheric processes, sufficient to increase or decrease the amount of precipitation in the required area of no more than 50,000 square kilometers, while the effectiveness of the impact is achieved by the resonant coincidence of the frequencies of the exciting wave with the frequencies of natural oscillations of the plasma of the sporadic layer and nonlinear effects

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SUBSTITUTE SHEET (RULE 26) electromagnetic radiation in the ionosphere caused by radiation generated in the pulse formation unit by electroacoustic and polarized quasi-constant electric fields. The method includes estimating the actual surface parameters (air temperature, relative air humidity, geopotential (at AT500 dam, AT850 dam), wind speed and direction (10 m, AT925dam, AT850dam, AT500dam, AT200dam) and space (plasma density, planetary index and field sign, X-ray intensity, earth rotation speed index, geomagnetic background variations, effective heights and frequencies of D,E,F1,F2) layers of weather for building a model of active effects, developing regulations and operating modes, as well as creating forecast data for surface changes weather for a period of at least 72 hours of the expected location and intensity of baric objects.The method includes electromagnetic action, which is carried out by pulses lasting from 150 milliseconds to 5 seconds, with an interruption duty cycle of at least 50 percent and no more than 11 pulses in a series of active effects - this ensures efficiency and environmental safety of the work performed. The method includes the synchronous application of the three devices of claim 1 when they are placed at a distance of 750 kilometers to ensure the effectiveness of the active impact. The method includes a single impact on the ionized layer at altitudes of 90-120 km, allows you to create ionized magnetic dipole formations in the atmosphere (troposphere), which allows you to carry out further active impacts to correct atmospheric processes at altitudes of 4-10 km.

The claimed method allows to carry out active influences on atmospheric processes in the interests of various branches of the national economy.

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SUBSTITUTE SHEET (RULE 26) households: improving water supply for agriculture or energy, reducing risks associated with hazardous phenomena such as frost, fog, hail, lightning, thunderstorms, etc.

The essence of the invention The present invention is a system for influencing weather processes in the Earth's atmosphere, containing a hardware unit for remote sensing of the atmosphere and ionosphere, an intelligent information processing unit, a unit for calculating the effective parameters of electromagnetic radiation and modulation parameters, as well as the radiation pattern and time of effective exposure to this radiation, command control unit, executive unit for active influence on meteorological processes in the Earth's atmosphere, made in the form of an antenna containing emitters of electromagnetic, optoacoustic, electric fields, combined into a single software and hardware complex with special software and mathematical software. In view of the foregoing, in accordance with the present invention, the components and blocks of the system connected via telecommunication channels for controlling and transmitting data to each other differ in that the block for actively influencing meteorological processes in the Earth's atmosphere is configured to provide a local change in the course of meteorological processes in the Earth's atmosphere with a radius up to 300 kilometers in the horizontal plane and to the height of the troposphere - in the vertical plane, while the emitter is configured to control the radiation pattern of the modulated radiation in accordance with the exposure parameters

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SUBSTITUTE SHEET (RULE 26) and corrections of the impact, determined in the block of means for remote sensing of the atmosphere and ionosphere, the block of intelligent information processing, the block for analyzing monitoring forecast meteorological information and the block for modifying weather conditions. In accordance with another feature of the present invention, the block of active influence on meteorological processes in the Earth's atmosphere is made in the form of a two-layer body, the outer one - consisting of high-alloy ferritic cast iron with desired properties and low magnetic permeability, which makes it possible to concentrate the usually lost magnetic component of the generated radiation inside the body itself, while the asphericity of the surface of the second-order body (conicoid) allows, in turn, to maximize the concentration of opto-acoustic resonantly modulated radiation when the wave front passes in the direction from the proximal to the distal surface of the radiator, which significantly increases the efficiency of the process and the internal - toroidal shape, made of composite electret material with given parameters of resonant polarization. In accordance with another property of the present invention, a cascade consisting of at least three electromagnetic bifilar coils with different frequencies close to the resonances of natural oscillations of ionized phases adjacent to the disturbed layers of plasma turbulence, modulated by the electronic- acoustic and optoelectronic devices. In accordance with another feature of the present invention, the active block is focused near the vertical direction, which allows electromagnetic pulses to reach the resonance region in the vicinity of the maximum concentration

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SUBSTITUTE SHEET (RULE 26) electrons at a height of 90-120 kilometers of the E-layer of the ionosphere, and the coincidence of the frequencies of the exciting wave with the frequencies of natural oscillations of the plasma makes it possible to achieve the desired effect, namely, the excitation of natural oscillations of the electron plasma and the development of plasma turbulence. The effect, insignificant in power, causes heating of the electron plasma, plasma structurization, acceleration of electrons, and due to the interference of the electromagnetic wave reflected from it, a standing wave is formed in the entire space between the excitation layer and the Earth's surface, generating the ability of active atmospheric aerosols to polarize or decay in the fields of electromagnetic radiation, self-organization aerosol magnetic dipole structures at the heights of determining the phase and group velocities of Rossby waves 10-16 km from the earth's surface, with further decay under the influence of gravity, atmospheric aerosols begin to function as water vapor condensation nuclei in the lower layers of the atmosphere, thereby contributing to the formation of cloud formation and precipitation centers . In accordance with another property of the present invention, the emitter is configured to control the radiation pattern of the modulated radiation in accordance with the parameters of the impact and adjust the impact, aimed at maintaining or destroying the above magnetic dipole formations in order to correct atmospheric processes associated with an increase or decrease in precipitation. In accordance with another feature of the present invention, during the process of polarization of water aerosols in the electric field of the atmosphere, a primary dipole moment of the aggregate of aerosol particles arises in the region of space covered by the electric field of an electromagnetic wave, leading to

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SUBSTITUTE SHEET (RULE 26) the emergence of cold plasma formations in the atmosphere. A feature of a plasma in a magnetic field is that, unlike conventional liquids and gases, in which there is only one type of wave - sound, a large number of various waves can exist in plasma, such as plasma, ion-sound, hybrid etc., this is the reason for the extremely large variety of nonlinear phenomena that occur during the combined resonant action in order to correct atmospheric processes. In accordance with another feature of the present invention, the method for correcting atmospheric processes provides for the preliminary construction of a model for the development of the synoptic situation in a given area, which includes two main approaches - discrete-event and process-oriented. The event approach is based on the formation of a program of operation modes with fixed parameters of impact at the time of the start of work, including the coordinates of the center of the impact area, the true azimuth, the polar pointing angle of the emitter unit, the time of switching on and off the system, not associated with a change in the synoptic situation for the entire period until the specified results. The process approach is based on the formation of changes in the processes that develop in the environment as a result of initial actions and is associated with changes in the synoptic situation that requires correction in the operating modes after each cycle of exposure. In accordance with another feature of the present invention, the objects of the system for modeling the correction of atmospheric processes are: astrogeophysical forecast, hydrodynamic forecast of the development of atmospheric processes, the composition and structure of the object, the properties of the elements and cause-and-effect relationships inherent in the analyzed object and essential for achieving goals, including

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SUBSTITUTE SHEET (RULE 26) changes in atmospheric circulation parameters, changes in the amount of precipitation, temperature regimes, a decrease in the level of fire risk, the filling of reservoirs, etc.

12. In accordance with another feature of the present invention, in order to serve a large area exceeding macroscale changes in atmospheric circulation, additional blocks of influence spaced apart at a distance of 750 kilometers can be included in the hardware-software complex, allowing mesoscale changes in atmospheric circulation to be carried out.

The present invention is illustrated by drawings and examples.

List of figures of drawings and other materials:

The present invention provides a new and effective method for correcting atmospheric processes, implemented using an active impact device, a hardware-software complex for analyzing and generating executive programs for combined electromagnetic radiation resonant with respect to ionized layers of the troposphere.

On fig. 1, an embodiment of the present invention is presented in the form of a block diagram illustrating an exemplary composition of a system connected via telecommunication channels for controlling and transmitting data to each other, processing data, making decisions and issuing executive commands in which the present invention can be implemented.

Figure 1 shows some of the advantages of the present invention, but as will be described below, the invention can be represented in

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SUBSTITUTE SHEET (RULE 26) several shapes, sizes, combinations of properties and elements, and with a different number of components and their functions.

The presented version of the hardware-software complex is implemented on an Internet platform that provides the organization of work on the correction of weather conditions and access to large databases and knowledge, combining information and computing components, contains an intelligent analysis system, a simulation system and an expert decision support system. Network 101, as shown in Fig. 1 includes connections 102a-p, which are the medium used to provide communication links between client and server, various devices and computers interconnected in network 101. Connections 102a-p can be wired or wireless connections. A few exemplary wired connections are cable, telephone line, and fiber optic cable. Examples of wireless connections include radio frequency (RF) and infrared (IR) transmission. Many other wired and wireless connections are known in the art and can be used concurrently with the present invention.

In this example, the network 101 includes a computer or mobile device with a pre-installed operator client program 104, an appliance 103, a server 105. The appliance can be used to execute programming instructions contained in software that can be obtained from the server 105 over a wide area network (WAN) 101. In one embodiment, the WAN is the Internet. Of course, the network 101 can also be implemented as a variety of different types of networks, such as, for example, an intranet, a local area network (LAN), or a cellular network. Rice. 1 is considered as an example and not as a structural limitation for the present invention.

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SUBSTITUTE SHEET (RULE 26) Server 105 can be thought of as a computer that manages access to a centralized resource or database. In some embodiments of the invention, the operator of the hardware-software complex 103 may request the functions and client part of the management of the complex, which is an example of the use of the present invention. The server 105 may receive, process and fulfill the request by transmitting the software application to the personal computing device 104 via the WAN/LAN, issue recommendations via the server 105 and WAN/LAN 101 directly to the operator 103.

Figure 2 shows a block diagram of a hardware-software analysis system, consisting of constituent elements and blocks structurally combined into a single complex that allows you to form the operating modes and control the device for actively influencing atmospheric processes.

Now let us turn to Fig. 2, in the above version, the software and hardware complex 103 consists of a block of means for recording and analyzing data from remote sensing of the atmosphere and electromagnetic background 201, including a digital meteorological station 201a and a recorder of levels of electrical and magnetic radiation 201 in surface control in the area of deployment devices and effects, a transceiver for sensing the speed of the ionosphere, a block for intelligent processing of information received via communication lines 202, a block for determining the effective parameters of electromagnetic radiation, modulation, this radiation, the radiation pattern and time of effective action 203, a command control block 204, an active influence block on meteorological processes 206 in the Earth's atmosphere, an ionospheric remote sensing unit 206 and an emitter unit 207 .

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SUBSTITUTE SHEET (RULE 26) On fig. 3 shows an embodiment of a device for actively influencing hydrometeorological processes illustrating its exemplary composition, the invention can be made in several shapes, sizes, combinations of properties and elements, and with a different number of components and their functions.

Now let's turn to fig. 3, in the above embodiment of the hardware-software analysis system, a function is provided for generating control commands for an active impact device consisting of a weather active impact unit 206 and an antenna emitter 207. This sketch allows illustrating the structural and functional features of the device described in the invention. The device for active influence on hydrometeorological processes consists of a generator of combined electromagnetic radiation 301, which includes six synchronized channels for controlling a block of emitters 302, which includes an outer case of an original design 303 of an aspherical second-order shape (conicoid), structurally consisting of high-alloy ferritic cast iron with desired properties and low magnetic permeability, an inner case toroidal shape 304, structurally consisting of a composite electret material with specified resonant polarization parameters and active electronic-acoustic and optoelectronic devices placed inside it, at least three electromagnetic bifilar coils 305 with different frequencies close to the resonances of natural oscillations of ionized phases are placed in the center of the block, adjacent to the disturbed layers of plasma turbulence. Rotary device 306 controlled via radio channels with a pointing accuracy in azimuth angle of at least 0.05 and zenith angle of at least 0.1 degrees, angular velocity of movement of at least 4.5 degrees per second and a working load of at least 50 kg. Block of switching and control of the device of active influence 307

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SUBSTITUTE SHEET (RULE 26) connected to the device by wire or using WiFi, Bluetooth channels.

The present invention is illustrated by examples of implementation.

Based on the appeal of the General Director of the Moscow Committee for Science and Technology in the period August-October 2010, the authors of the invention carried out research work on active influences on atmospheric processes in order to normalize the environmental situation and increase precipitation in three agreed regions.

The purpose of experimental studies: performance of work using the method of correcting atmospheric processes, meteorological and electrical parameters in the troposphere using the Active Influence Device according to claim 1 and the hardware-software analysis system according to claim 4.

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SUBSTITUTE SHEET (RULE 26)

Example 1

Experiment tasks:

- Freeing the air basin of the Moscow region from smog, enhanced by the smoke of forest and peat fires, using the method of changing the direction of movement of air masses, with a predominance of the western wind direction;

- the destruction of the blocking anticyclone with the center in the Moscow region, the displacement of the cyclone, which carries out a large-scale removal of the hot air of Asia Minor;

- decrease in temperature in a given region;

- restoration of zonal transfer of air masses over a given territory, prevention of hurricanes over the serviced territory.

Experimental work was carried out on the contractor's area in the city of Lytkarino, Moscow Region, located at an altitude of 143 m relative to sea level. Beginning and end of experimental studies on August 08, 2010. and August 18, 2010, respectively.

Active Influence Device:

Breadboard sample of the device 01 pcs.

The composition of the hardware-software analysis system:

- to measure the electrical parameters of the atmosphere

■ stationary measuring device for air conductivity

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SUBSTITUTE SHEET (RULE 26) type "Electrical conductivity - 2";

■ portable device type ST-01 for measuring electric field strength;

■ device type ST-1, which determines the concentration of light ions.

- to determine the meteorological parameters of the atmosphere and meteorological formations:

• cloud base meter of IVO type;

• instrument type 1V1-63 DNI for measuring wind speed and direction in the surface layer of the atmosphere;

• a device for measuring air humidity;

• thermometers installed at ground level;

• devices for measuring background radiation;

• mercury barometer to measure pressure;

• meteorological radars designed to determine the parameters of the radio echo of clouds and precipitation, as well as to determine the speed and direction of their displacement;

• radiometers for determining the moisture content of the atmosphere and water content.

At the time of the start of the experiment on August 08, 2010, an emergency environmental situation had developed in Moscow - the strongest smog, the concentrations of pollutants in Moscow exceeded the maximum permissible concentrations several times: for carbon monoxide - up to almost 7 times, for suspended solids - up to 16 times, according to nitrogen dioxide - more than 2 times. The smog was caused by wildfires

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SUBSTITUTE SHEET (RULE 26) due to the abnormally hot weather that began in the last ten days of June, in terms of duration and degree of consequences, it had no analogues in more than a century of weather observations. The heat in the Moscow region was determined by a vast, slow-moving blocking anticyclone, which settled down to a height of about 16 km (in the troposphere and lower stratosphere), with a center in the area of the experiment, which disrupted normal western transport.

On the days of the experiment, the following meteorological information was received and analyzed:

- synoptic weather maps;

- ring weather maps;

- baric field on AT 500/1000;

- rolling weather forecasts for 6 days (Exektr (UKMO), NOGAPS, GMTsRF);

- the actual state of the weather.

The data of background values of electrical parameters in the surface air layer were recorded;

- actual intensity of electric and magnetic fields, data on ion concentration;

- moisture content of the atmosphere above the location of the device.

The frequency of observations is determined by the purpose of the experiment and is established after determining the temporal changes in atmospheric formations, meteorological and electrical parameters of the atmosphere on the day of testing.

Based on the data of the hardware-software analysis system, a program of work performed by the device was compiled to reduce the height of the tropospheric turbulent layer south of Moscow at a distance of 1250 km and increase the electron concentration layer to the northwest at a distance of 1250 km. When coordinating the program at an altitude of AT 500 and the surface layer of atmospheric pressure, it was supposed to change the circulation regime from the predicted one (Fig. 4.). On August 09, 2010 the experiment was started.

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SUBSTITUTE SHEET (RULE 26) Below, in graphical form, are presented the prognostic and actual maps of the AT 500 geopotential for the period of the experiment, which are freely available on the website of the company wetheronline.UK., graphs of changes in temperature and chemical parameters of air.

On August 18, as it was envisaged by the experiment program, the blocking anticyclone was destroyed, and the second stage of restoration of zonal transfer began. At the same time, the ongoing work on a smooth change in the temperature regime made it possible to avoid catastrophic hurricanes predicted when changing contrasting air masses.

Example 2

Experiment tasks:

- extinguishing natural and man-made fires by creating sedimentation in areas with a large number of combustion centers of the central federal district (Moscow, Ryazan, Vladimir, Nizhny Novgorod, Voronezh, Lipetsk regions).

Experimental work was carried out on the areas of the contractor in the city of

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SUBSTITUTE SHEET (RULE 26) Lytkarino, Moscow region, located at an altitude of 143m. relative to sea level. Beginning and end of experimental studies on August 18, 2010. and August 28, 2010, respectively.

Active Influence Device:

Breadboard sample of the device 01 pcs.

The composition of the hardware-software analysis system:

- to measure the electrical parameters of the atmosphere

■ stationary device for measuring air conductivity of the type "Electrical conductivity - 2";

■ portable device type ST-01 for measuring electric field strength;

■ device type ST-1, which determines the concentration of light ions.

- to determine the meteorological parameters of the atmosphere and meteorological formations:

• cloud base meter of IVO type;

• instrument type 1\1-63 DIL for measuring wind speed and direction in the surface layer of the atmosphere;

• a device for measuring air humidity;

• thermometers installed at ground level;

• devices for measuring background radiation;

• mercury barometer to measure pressure;

• meteorological radars designed to determine the parameters of the radio echo of clouds and precipitation, as well as to determine the speed and direction of their displacement;

• radiometers for determining the moisture content of the atmosphere

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SUBSTITUTE SHEET (RULE 26) and water supply.

At the beginning of the experiment on August 18, 2010, a difficult fire situation developed in the served territory of Russia due to abnormal heat and lack of precipitation, according to the Ministry of Emergency Situations of the Russian Federation, the fire area was more than 500 thousand hectares. 831 fires were registered, including 42 peat fires. (Fig.5)

On the days of the experiment, the following meteorological information was received and analyzed:

- synoptic weather maps;

- ring weather maps;

- baric field on AT 500/1000;

- sliding weather forecasts for 6 days (Exektr (UKMO), NOGAPS, HMC RF);

- the actual state of the weather.

The data of background values of electrical parameters in the surface air layer were recorded;

- actual intensity of electric and magnetic fields, data on ion concentration;

- moisture content of the atmosphere above the location of the device.

The frequency of observations is determined by the purpose of the experiment and is established after determining the temporal changes in atmospheric formations, meteorological and electrical parameters of the atmosphere on the day of testing.

Based on the data of the hardware-software analysis system, a program of work performed by the device was compiled in order to reduce the height of the tropospheric turbulent layer west of Moscow, at a distance of 1550 km (Fig. 6), in order to change the trajectory of the Atlantic cyclones at a height of 2-4 km., directly over territories

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SUBSTITUTE SHEET (RULE 26) engulfed in fires.

The actual maps of geopotential AT 500 at the beginning and end of the ongoing work, placed in free access, are presented in graphical form below, characterizing the formation of a low-pressure trough in the impact zones. (Fig.7)

According to the hydrometeorological center, as a result of ten days of work, from 130 to 330% of the ten-day rainfall in the region fell over the serviced area, the data presented in Fig. 6. In Moscow and the region, precipitation amounted to 62 mm, according to the Ministry of Emergencies, a decrease in the fire hazard situation is achieved with 28 mm of precipitation. Thanks to the work performed, forest fires were extinguished. (Rie.8)

A report on the work performed is presented to the customer.

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SUBSTITUTE SHEET (RULE 26)

Claims

FORMULA A device for active influence on hydrometeorological processes, consisting of a generator of combined electromagnetic radiation of the optical and radio frequency spectrum, and a block of emitters of low-intensity electromagnetic pulses modulated by acoustic, optical and polarized quasi-constant electric fields, located on a rotary device and made in a single two-layer housing, the outer layer is aspherical of the second order (conicoid), made of highly alloyed ferritic cast iron with specified properties and low magnetic permeability, the inner layer of a toroidal shape is made of a composite electromagnet oi'o material with specified resonant polarization parameters, which makes it possible to effect resonant radiation focused near the vertical direction to turbulent layers of the lower ionosphere based on programs coming from the control unit via wired and wireless communication channels. The block of emitters according to claim 1 is made in the form of a cascade consisting of at least three electromagnetic bifilar coils with different frequencies close to the resonances of natural oscillations of ionized phases, in the ranges of 200-1600 kHz, 1-8 MHz, 2-16 GHz, adjacent to perturbed layers of plasma turbulence, modulated by the electronic-acoustic and optoelectronic devices included in the block of active influences according to the frequency of the spectrum of harmonic oscillations of the Schumann resonance. The device control system according to items 1-2, consisting of components and blocks structurally combined into a single complex, including a unit for analyzing actual data and physical predictors of meteorological and heliogeospace parameters, a unit for generating executive operating modes and a device control unit according to item 1 ,2 , which allows to process the data of the recorded parameters, to identify, on the basis of artificial intelligence, the signs and microphysical characteristics required for the formation of executive work programs in automatic mode and to transmit using a processor to a rotary device and a generator of combined electromagnetic radiation of the optical and radio frequency spectrum. The system according to claim 3, characterized in that the analysis unit includes a digital meteorological station and a recorder of electric and magnetic radiation levels designed to assess changes in physical parameters in the surface layer and a database of space weather parameters obtained from open Internet sources. The system according to claim 3 is characterized in that the block for generating the executive modes of operation includes the start time and duration of exposure, the choice of the number of emitters involved, the modulation mode of the emitter signals in frequency and amplitude, the determination of the azimuth and focus angle of the block of emitters transmitted to the rotary device. A method for correcting atmospheric processes using the device of claim 1, including an active impact on the area the maximum concentration of electrons in the ionospheric layer with a height of 90-120 kilometers, the creation and development of plasma turbulence of different directions, the change in thermobaric gradients in atmospheric processes, sufficient to increase or decrease the amount of precipitation in the required area of not more than 50,000 square kilometers, while the effectiveness of the impact is achieved by resonant the coincidence of the frequencies of the exciting wave with the frequencies of natural oscillations of the plasma of the sporadic layer and the nonlinear effects of electromagnetic radiation in the ionosphere caused by radiation generated in the pulse formation unit by electroacoustic and polarized quasi-constant electric fields with a duration of 150 milliseconds to 5 seconds, an interruption duty cycle of at least 50 percent and no more 11 impulses in a series of active actions, the method according to item 6, characterized in that the actual surface weather parameters are evaluated (air temperature, relative humidity air, geopotential (at altitudes AT500dam, AT850dam), wind speed and direction (10 m, AT925dam, AT850dam, AT500dam, AT200dam)) and space weather (plasma density, planetary index and field sign, X-ray intensity, rotation speed index earth, geomagnetic background variations, effective heights and frequencies of layers D, E, F1, F2), after which, according to the data obtained, a model of active effects is built and the regulations and operating modes are developed, followed by the determination of forecast data for changes in surface weather for a period of at least 72 hours of expected location and intensity of baric objects. The method according to claims 6, 7, characterized in that the effectiveness of the active impact can be increased due to the synchronous use of the three devices of claim 1 when they are placed at a distance of at least 750 kilometers. The method according to p.p. 6.7, characterized in that a single impact of a pulse on the ionized layer at altitudes of 90-120 km ensures the creation of ionized magnetic dipole formations in the atmosphere (troposphere) and correction of atmospheric processes at altitudes of 4-10 km.