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Gadget to measure sea wave parameters |
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IPC classes for russian patent Gadget to measure sea wave parameters (RU 2523102):
Device of determination of distance to ionosphere / 2510772
Device of determination of distance to ionosphere can be used in over-the-horizon radars and for research of a status of an air bed of Earth. The specified result is reached with the help of a synchroniser, a pulse transmitter, an antenna switch, an aerial, a receiver, a clock generator, a decoder, a block of secondary processing, an indicator, a peak selector, a variable line of delay, a block of fixing of a certain duration of a forward part of a signal, an analyser of the smallest range, an adder, a panel of delivery of a code of the delay, connected among themselves definitely.
Method for early detection of atmospheric vortices in clouds using noncoherent radar / 2503030
Detection of cyclonic vortices in thunder clouds using noncoherent radar involves radar probing of the cloud at wavelength of 10 cm, determining reflectivity at given spatial points of the cloud environment, and displaying said data on the screen of a personal computer in form of a three-dimensional radar image of the cloud; the obtained image of the cloud is viewed from all sides on the background of the screen of the personal computer in dynamic mode, removing, during each view of the three-dimensional image, the external envelope which corresponds to a 2 dBZ drop in radar reflectivity; upon detecting a contour of the presumed cavity of the atmospheric vortex on the surface of the image, the image is viewed on the background of the screen of the personal computer and if the colour of the detected cavity matches that of the background of the screen of the personal computer, said cavity is identified as the cavity of the atmospheric vortex.
Radar method of determining parameters of large-scale wave on water surface / 2501037
Radar method of determining parameters of a large-scale wave on a water surface using a radio altimeter involves emitting probing pulses vertically downwards towards the water surface (to the nadir), receiving probing pulses reflected from the water surface, recording their shape and determining the height of the large-scale wave on the water surface from the inclination of the leading edge of the reflected pulse. Measurements are taken using an aircraft-mounted compact satellite radio altimeter with a knife-edge beam directed along the direction of flight, and the inclination of the trailing edge of the reflected pulse, taking into account the altitude of the aircraft and the antenna beam width, is used to determine variance of the inclination of the large-scale wave along the direction of flight, and the average length of the surface wave along the flight direction is determined using the measured variance of inclination and height of the large-scale wave on the water surface.
Method for radar measurement of cloud and precipitation particle charge / 2491574
In the disclosed method, the region of the atmosphere under investigation is simultaneously irradiated with an electromagnetic wave with wavelength λ1, which is not damped during propagation in the investigated medium, and a wave with length λ2, which is damped; reflected electromagnetic signals from two volumes lying within the investigated region are received; power of the electromagnetic signals reflected from the first and second volumes, as well as phase shift between said signals are measured separately and the measurement results are used to determine the cloud and precipitation particle charge of the investigated region using the formula:
Portable remote measuring device for parameters of oil layer spilled on water surface / 2478915
Device includes two radiometric receivers of microwave range, which operate on frequencies corresponding to transparent windows of atmosphere. Each receiver includes an antenna, a polarisation switch, a high-frequency unit with a synchronous detector and corresponding control circuits. Measuring zones of radiometric receivers of microwave range are put in each other due to their corresponding arrangement on the load-carrying structure. At that, measuring zone of parameters of more high-frequency receiver is fully located inside the measuring zone of low-frequency receiver. Device also includes a two-coordinate inclination compass, a computer, a radiometric receiver of IR-range, a video camera, a GSM-modem, a GPS-receiver and a LED projector.
Method of adjusting output parameters of superregenerative transceiver of radiosonde / 2470323
Invention relates to radio engineering and can be used to adjust sensitivity and relative position of the receiving and transmitting frequency of superregenerative transceivers of aerologic radiosondes operating as part of atmospheric radiosounding systems. Disclosed is a method of adjusting output parameters of a superregenerative transceiver of a radiosonde based on optimum selection of the feedback factor of the self-oscillator of the superregenerative transceiver, load resistor, resonance frequency of the oscillatory system, characterised by that when launching the self-oscillator of the superregenerative transceiver, a mode for self-excitation with a hard character of the transient process of establishing self-oscillations is provided, average current and supply voltage of the active device of the self-oscillator of the superregenerative transceiver are stabilised, pulsed current of the control electrode - base of the transistor of the active device of the self-oscillator is controlled, thereby establishing reception frequency relative the carrier frequency of the self-oscillations of the superregenerative transceiver; by adjusting the slope of the exponentially rising leading edge and pulse duration, the required level of sensitivity of the superregenerative transceiver is set.
Device for measuring vertical component of wind velocity for detecting wind shift / 2468387
Device for measuring the vertical component of wind velocity in order to detect wind shift has a wind shift detector, a transmitter, two receivers, two circulators, two antennae, a digital signal processor, an antenna angular position sensor, a cross-correlation function derivative computer, a device for determining the position of the minimum of the cross-correlation function derivative, a power divider, a differentiator, an adjustable delay unit, a multiplier, a low-pass filter and a low frequency amplifier.
Method of estimating accuracy of doppler radar wind profile / 2460091
Method of estimating accuracy of Doppler radar wind profile (DRWP) includes one radiosonde radar weather station, based on synchronous probing of the atmosphere by the DRWP and a standard meteorological apparatus (MA), where the speed and direction of wind are measured, the DRWP and MA obtain several results which are fed to a computer. The mean-square error of the DRWP in measuring speed and direction of wind is determined based on equal accuracy of measurements with given confidence probability. The disclosed invention is characterised by making the MA in form of two identical radiosonde radar weather stations, the wind speed and direction measurement results of each of which form the first outputs are fed to the second and third inputs of the computer where they are averaged. The difference in results is taken, transformation is performed and the accuracy of the DRWP in measuring speed and direction of wind is determined based on a corresponding mathematical relationship.
Method of determining sea ice draft and system to this end / 2453865
Invention relates to marine hydrometeorology and may be used for determination of sea ice draft. Drifter equipped with transceivers of satellite communication and hydro acoustic navigation systems is used to define coordinates of ice fields. Displacement of ice field relative to reference points is tracked and displayed on monitor. Note here that potentially dangerous ice fields are revealed as well as approach distance and time store to make decision about their localisation. Said decision are made with due allowance of ice field thickness defined by sounding with the help of sonar mounted aboard the airship. Proposed system comprises drifter, producing offshore platform and sonar mounted on rigid-frame airship. Drifter is made up of telescopic cylindrical vessel made from Macrolon. Drifter top section accommodates aforesaid transceiver while it bottom section houses transceiver of hydro acoustic hardware. Said drifter operateds in ''call-reply'' mode and ''pinger'' mode (beacon). For reliable fixing of drifter in holes on ice surface, spacers made up of set of needle passages are made at top section of cylindrical vessel. Producing offshore platform is equipped with transceivers of aforesaid systems, antennas, navigation controller and software. Said sonar mounted aboard the airship serves to define ice field thickness.
Panoramic radar method of determining parameters of state of ocean surface layer from satellite / 2449312
Knife-edge beam of the antenna is rocked relative the vertical in a direction perpendicular to the direction of motion and each probe pulse is used to illuminate a 14x355 km spot on the water surface (at altitude of 800 km). Reflected pulses are received using time gating on the range based on the Doppler shift sign to select in said 14x355 km spot elementary scattering cells (ESC) measuring, for example, 14x14 km. Using a synthesis procedure along the direction of motion of the satellite, the backscattering section is determined and the water surface slope dispersion in each ESC is reconstructed. Further, by selecting the azimuth angle, the water surface slope dispersion along said direction is reconstructed and, by analysing the azimuth dependency of slope dispersion in each ESC, the direction of wave propagation in each cell is determined. The speed of surface wind V in each ESC is determined using an algorithm obtained using a regression method. In a special case of the method, average values of the rough sea and wavelength of a big wave are also determined.
Method nd device for measuring electron concentration at specific region of ionosphere / 2251713
Method and device can be used for measuring concentration of electrons in specific region of ionosphere plasma which depends on presence and concentration of radioactive impurities in the region of atmosphere to be observed. Device has synchronizer 1, transmitter 2, transmitting aerial, time delay unit, two receiving aerials, right and left circular polarization wave receivers, two switches, heterodyne, mixer, intermediate frequency amplifier, five multipliers, narrow band filter, amplitude limiter, phase meter, computing unit, comparison unit, indicator, phase shifter, scaling switch, subtracter and adder.
Method for determination of location of lightning discharge and multiple-point system for its realization / 2253133
The multiple-point system for determination of location of a lighting discharge has a data transmission network and sensors, central computing unit, control unit and user computers (according to the number of users) connected to it, superlong-wave independent lightning direction finders - range finders are used as sensors.
Method for measuring thickness of snow cover / 2262718
Method is based physically on different penetrability level of snow by electromagnetic waves of different frequencies ranges, which is connected to dielectric snow characteristics. Method for measuring thickness of snow covering includes irradiation of snow cover at the same time by electromagnetic waves of centimeter range on bearing frequency f1, on which reflection occurs from limit between snow and soil, and electromagnetic waves of optical range on bearing frequency f2, on which reflection occurs from limit of separation of environments troposphere-snow, and determining of appearing difference of distances, passed by proving signals.
Mode of sounding of atmosphere or ocean / 2267139
The technical result: simplification of realization of measuring, increasing their precision and also securing possibility of independent definition as the profile of the speed of the sound, so the profile of the index of reflection in atmosphere or in ocean. The essence: in the environment a movement of a sounding object is set up, a modulated acoustic or electromagnetic wave is directed on this object. The wave holds frequencies f1 and f2 and f1≥C/h and f2≤C/H, where C - a medium speed of the wave in the investigated environment, h - required space permission, H - a maximum distance of measuring, reradiated by the object. Corresponding relative Doppler shifts at various locations of the object are defined for frequencies f1 and f2 reradiated by the object. Attitude for these shifts is found. According to this attitude the vertical profile of the speed of the propagation of the wave is computed. Particularly an acoustic wave packet is chosen in quality of sounding object and a vertical profile of the speed of propagation of the electromagnetic wave is computed. The profile of the speed of the sound is defined along the profile of the shift of the frequency f1 with taking into account the profile of the speed of propagation of the electromagnetic wave. Particularly for various moments of time an integral shift of the phase of the wave reradiated by the object on the carrier frequency is found and along this shift a slant distance till sounding object is defined. Particularly along the parameters of received signals an azimuth and an angle of the place of the sounding object are found.
Storms coordinates accumulator and a variant thereof / 2269792
Kinematic communication equations are solved not for aircraft-lighting flashes, but for aircraft-storm, and because storm coordinates are generated by averaging coordinates of all registered lightning flashes during several minutes, volume of computational operations is decreased manifold.
Panoramic radar method of determining condition of ocean's layer surface from satellite / 2274877
Method can be used for measuring parameters of sea storm; it can be also used in meteorology and oceanology for distant probing of surface layers of oceans from board of satellite. Microwave range probing pulses are irradiated by Doppler radar. Probing pulses are directed to surface of ocean in nadir; any pulse irradiates spot with sizes of 14x355 km on water surface. When receiving reflected pulses, time and Doppler range selection is used simultaneously inside spot of 14x355 km for elementary dissipating particles with sizes of 14x14 km. Then cross-sections of back dissipation σ0(θi) and σ0(θi+1) are determined for any two sequent "I"-th and "i+1"-th elementary dissipating particles. The cross-sections correct and determine dispersion of inclinations σ2 i(φj). The total dispersion of inclinations σ2 i for "i"-th elementary dissipating particles is determined and direction of propagation φwi of large-scale storm in "i"-th elementary dissipating particle is found. Speed V of surface wind is found by means of algorithm f V=F[σo, σ2 i(φj), σ2 i(φj+90°)] calculated by standard regression method.
Combined inbuilt control system and a variant thereof / 2277716
Combined inbuilt control system and its variant for storm locators, working in area of very low frequency electromagnetic fields, provides automatic, continuous control with given frequency of electric and magnetic antennas and storm detector channels appropriate for these by creating electric and magnetic fields, distributed in time, to make it possible to perform selection of lightning discharge pulse in two variants of selector circuit construction and to block control circuit automatically for time of lightning discharge pulse processing. Utilization of combined inbuilt control system in equipment makes it possible to increase fullness of storm locator control due to controlling through space of both magnetic and electric antennas, while preventing miss or distortion of lightning discharge processing pulse results when it coincides in time with control pulse.
Super regenerative transceiver / 2291467
The super regenerative transceiver has a generator of superior impulses, a master oscillator, a source of feeding and an antenna. At that there is introduced in it a diode and in series introduced a line out of a constant resistor, an alternate resister and a condenser. At that the input of the line is connected with the output of the generator of superior impulses, the output - with the input of the launching of the main oscillator, and the common point of the constant and the alternate resistors is connected with null volt of the source of feeding through directly switched diode, the generator of superior impulses and the main oscillator are connected with the plus and the null of the source of feeding, and the output of the main oscillator through antenna is the output of the super regenerative transceiver.
Method of measuring size of hail's particles / 2292565
Sizes of hail particles are measured by means of two-wave meteorological radar. Radio location probing of atmosphere is carried out within area of precipitation. Radio location reflectivity is determined at wavelengths of 3,2 cm and 10 cm, which equals to η3,2 and η10. Sizes of hail particles is calculated by relation of d3=4,54(η3,2/η10) -0,502, where 4,54 and -0,502 are empiric coefficients. Path of melting of hail particles is determined by radio location method when particles move in atmosphere from zero isotherm level down - H (km). Sizes of hail particles to be found is determined by multiplication of calculated value d3 by correcting multiplier K, found from relation of K=Ha(η3,2/η10)bH, where a=-0,247 and b=0,055.
Mode of definition of the width of the spectral density of power of radio signals of coherent meteorological radar / 2293351
According to the mode it is necessary to radiate periodically radio impulses into the researched field of atmosphere, to receive radio signals reflected from meteorological particles, to separate coherent and quadrature components of received radio signals reflected from meteorological particles, to form a complex signal uniting coherent and quadrature components of received radio signals reflected from meteorological particles, to calculate the correlation function of the complex signal. The indicated function is calculated in time points the intervals between whom are multiple to the period of repetition of radio signals. The width of the spectral density of power of the radio signals of the coherent meteorological radar reflected from meteorological particles is defined according to the relation:
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FIELD: instrumentation. SUBSTANCE: invention relates to instrumentation and can be used in meteorology, navigation, oceanography, vessel and seaplane sea trials for estimation of wave roughness and computer-aided landing systems. This gadget comprises antenna 1, transceiver 2, Doppler signal amplifier 3, ADC 4 and computer 5 its second input being connected with gadget input 6 and first output connected with transceiver control input. Besides, the gadget is equipped with display 7 with input connected to second output of computer 5. EFFECT: simplified hardware, higher reliability, fast response and precise calculation. 1 dwg
The present invention relates to measuring technique and can be used in meteorology, navigation, Oceanographic research, operational tests of ships and seaplanes to evaluate the strength of the agitation of the waves, in the automated landing systems of amphibians on the water surface in the daytime and night time. The known device for determining parameters of the waves that are protected by patents of the Russian Federation No. 416563, CL G01C 13/00, 1971, No. 349683, CL G01C 13/00, 1974, containing the receiver hydrostatic pressure electroprecipitation, zero-body, the comparison circuit, the generator of time averaging filter and the indicator. The operation of this device is based on the contact transformation pressure of sea waves into an electrical signal and further measurements of this signal. Signs, General signs of the claimed device, these devices are averaging filter and the indicator. Factor hindering the achievement of these devices technical result provided by the invention, is a fairly narrow scope, due to the need of a contact transformation pressure of sea waves into an electric signal. It is also known a device for measuring the parameters of the waves, protected by the RF patent №726422, CL G01C 13/00, 1977, containing PR is EMPRETEC with the antenna zero-body, the comparison circuit, the generator of time averaging filter and the indicator. This device is a contact transformation of the waves replaced by contactless using the transceiver. Signs of this analogue, in common with the features of the proposed device is a transceiver with an antenna, averaging filter and the indicator. The obstacles to achieve this similar technical result provided by the invention are the limitations of the field measured parameters and the relatively low accuracy of their measurement. It should be noted that these disadvantages inherent in the devices protected by the RF patents №№416563 and 549683. The closest to the technical nature of the claimed (prototype) is a device for measuring the parameters of the waves, protected by the RF patent №2036429, CL G01C 13/00, 1990, It contains a transceiver with antenna, power Doppler signal, indicator and autocorrelator, which includes a mixer, a delay line with taps, switch, averaging filter, a comparator, a pulse generator, a pulse counter, a decoder and a control key. Signs, General signs of the inventive device, the device of the prototype are transceiver with antenna, power Doppler signal and indicator. Working prototype based the on the radiation of the sea surface by radio pulses with constant parameters, the selection of the radar (reflected from the sea surface) of the Doppler signal component determined by the speed of movement of the waves, the definition of the autocorrelation function of this component and measuring the time decay of this function from the maximum value to zero. This time characterizes the degree of rough seas and in principle can be translated into points on the Beaufort scale. The time decay of the autocorrelation function of the maximum value to zero is displayed on the indicator. The obstacles to achieve your prototype technical result provided by the invention are relatively low precision, performance and reliability of prototype. This is because autocorrelator performed analog and contains a sufficiently large number of elements that makes it difficult, and hence adversely affects its reliability. Itself analog implementation of autocorrelator is not possible to realize high-precision calculation of the correlation function, and the presence of an analog block that performs the function of the averaging filter, requires the implementation of this function a considerable investment of time. Another factor hindering the achievement in prototype technical result provided by the invention are dostat is a rule limited functionality of the prototype. It allows you to define only the autocorrelation function of the Doppler component reflected from the sea surface signal and the decay time of this function from maximum to zero level. This time, in fact, is the measurement result is reflected on the display. It is not enough to fully characterize marine excitement. For a more complete characterization of the agitation of the sea surface, it is desirable to have the full autocorrelation function of the Doppler component reflected from the sea surface signal and its spectrum and distribution law. To obtain these characteristics, the device is a prototype. Technical problem on which the invention is directed, is to simplify and expand the functionality of the device and improve its performance, accuracy and reliability. To achieve the technical result in the known device for measuring the parameters of the waves, containing the transceiver with antenna, power Doppler signal, an input connected to the output of the transceiver, and the indicator is entered serially connected analog-to-digital Converter, whose input is connected to the amplifier output Doppler signal, and the transmitter, a second input which is the input of the first output connection of the EN with the control input of the transceiver, and the second output to the input of the indicator. There are no sources of information, in which the newly introduced elements would be described in conjunction with the other elements of the claimed device. Therefore, the proposed device should be considered to be new and involve an inventive step. The invention is illustrated by the drawing, which shows the structural diagram of the inventive device. The device comprises a series-connected antenna 1, the transceiver 2, the amplifier 3 Doppler signal, analog-to-digital Converter 4 and the computer 5, the second input is connected to the input 6 of the device, and the first output with the control input of the transceiver. In addition, the device has an indicator (display) 7, an input connected to the second output of the transmitter 5. The operation of the device is as follows. Transceiver 2 generates and transmits via the antenna 1 in the direction of the sea surface radio pulses probing signal with the given parameters. The parameters of the probing signal (power, duration, duty cycle, carrier frequency) produced by the transmitter 5 in accordance with the altitude of the carrier device, the code which is fed to the input 6 of the device. Developed by the evaluator 5 set the parameters of the probing signal received from the first you is an ode to the control input of the transceiver 2. Reflected from the sea surface, radiated sounding signal is transformed into an echo signal having a random character. He is received by the antenna 1 and fed to the receiver of the transceiver 2, where it is divided Doppler component due to the movement speed of the waves. This component from the output of the receiver of the transceiver 2 to the input of the amplifier 3. In the amplifier 3 received at its input signal is further filtered (from it are only the Doppler frequency, is amplified and fed to the input of the inverter 4. In the Converter 4 analog Doppler signal is converted into digital form (quantized), i.e. converted into a sequence of separated from each other by time t on the quantization step ∆ T digital codes corresponding to the levels found at this step the input analog signal. Step Δt quantization in accordance with the Nyquist theorem is selected:
where Fmaxmaximum frequency in the spectrum of the Doppler signal. From the output of the Converter 4 is converted into a sequence of digital codes Doppler signal is fed to the input of the transmitter 5. In calc, the body 5 is calculated from the histogram distribution of the numerical values received at its input digital codes, the corresponding probability density functions of the current level of x(t) of the Doppler signal (distribution law). In addition, the calculator 5 calculates the autocorrelation function of Rx:(τ) Doppler signal x(t). The calculation is carried out in accordance with the equation:
where τ is the argument of the autocorrelation function, i.e. the time delay between the test signal and its copy. Feature on the product x(t)·x(t+τ) means averaging. The transmitter 5 is calculated spectrum (spectral density) Sx(ω) Doppler signal x(t)associated with the correlation function Rx(τ) Fourier transform:
The device is quite easy to implement is. As the transmitter 5 can serve as the on-Board computer media devices. The calculation results can be obtained in the form of tables and graphs. They are submitted for indicator 7, which can be used to display, through which the programming and debugging programs that implement the described calculations. As other elements of the device can be used the same elements as in the device prototype. It is easy to see that in the inventive device in comparison with the prototype significantly reduced hardware part, because the analog performance of autocorrelator replaced by additional programming of the computer, which is usually already included in the media device. The reduction of the hardware structure of the device significantly simplifies and enhances reliability. In addition, it increases the speed and accuracy of calculation of the autocorrelation function as a computer, working with signals in digital form allows you to perform all the calculations faster and more accurately than analog autocorrelator implemented on the physical blocks (mixer, a delay line with taps, switch, averaging filter, driven key, comparator, pulse counter, decoder). It is also obvious that the functionality of the inventive device is considerably wider than the devices of the prototype, as it allows not only to determine the decay time of the correlation function from maximum to zero, and all of the correlation function. In addition, it allows you to identify and reflect on the display screen as the correlation function and the distribution and spectrum of the Doppler signal. Device for measuring parameters of the waves, containing the transceiver with antenna, power Doppler signal, an input connected to the output of the transceiver, and a display, characterized in that it introduced serially connected analog-to-digital Converter, whose input is connected to the amplifier output Doppler signal, and the transmitter, a second input which is the input of the first output is connected with the control input of the transceiver, and the second output to the input of the indicator.
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