75 results about "Total electron content" patented technology

An embodiment of the invention discloses a hyper-spectral estimation model constructing method of total nitrogen content of rice leaves. The method comprises steps as follows: multiple experimental plots are selected, and multiple sampling points are selected in each experimental plot; canopy spectral measurement is performed at the critical growing stage of rice; multiple sampling spectrums are recorded at each sampling point, and an average value is taken as a spectral measurement value of the sampling point; a hyper-spectral image of each experimental plot is acquired by an airborne imaging spectrometer; multiple function leaves at different parts are collected at each sampling point, and the total nitrogen content of the rice leaves is measured; the hyper-spectral estimation model of the total nitrogen content of the rice leaves is constructed with the adoption of spectral indexes or a partial least-squares regression method. The embodiment of the invention further discloses a hyper-spectral estimation method of the total nitrogen content of the rice leaves. The total nitrogen content of the rice leaves is estimated according to the model constructed with the method. The scientific and technical basis can be provided for space inversion of the nitrogen content of regional-scale rice and efficient implementation of precision agriculture.

Calibrating a receiver for a satellite positioning system. At preset intervals, a plurality of calibration signals are generated and applied to the receiver. The plurality of calibration signals correspond to a plurality of satellite signals, respectively, from the satellite positioning system. A relative time-delay bias from a delay estimation algorithm within the receiver. The time-delay bias is stored, preferably with the receiver. The receiver receives the plurality of satellite signals from the satellite positioning system. The plurality of satellite signals are processed with the time-delay bias. The processing reduces effects from the satellite receiver and improving estimate of the differential delay and total electron content (TEC).

The invention discloses a GNSS ionization layer delay precise modeling method suitable for a Chinese region. The geographical coordinates of the latitude and the longitude of a cross point are converted into coordinates under an established spherical crown coordinate system, so as to acquire the range of the latitude and the longitude of the cross point under the spherical crown coordinate system. The change range of the latitude and the longitude of the cross point is projected and converted into a global coordinate system. A spherical harmonic function is used to establish a regional ionization layer total electron content (TEC) model. The ionization layer delay precise modeling method suitable for the Chinese region is constructed. Compared with the existing method, the method provided by the invention has the advantages that through rotation projection and conversion, the distribution of the ionization layer cross point meets the requirement of the spherical harmonic function on physical quantity distribution in the form; ill-conditioned problems are solved when the spherical harmonic function is applied to regional modeling; the precise describing ability of the spherical harmonic function for global change physical quantity is effectively used; non-integral order in a spherical crown harmonic function is avoided; and the complexity of ionization layer TEC modeling calculation is reduced.

The invention discloses an optical module for a wide temperature range and a working temperature adjusting method thereof. The optical module comprises a laser transmitting unit, an MCU (microprogrammed control unit) and a TEC (total electron content) control circuit, wherein the laser transmitting unit comprises a laser and a drive circuit; the optical power of the laser is previously calibrated to the specific optical power range; the MCU is used for determining the working temperature setting value corresponding to the acquired temperature value after acquiring the temperature value detected by a temperature sensor; and the TEC control circuit is controlled to adjust the working temperature of the laser at the corresponding temperature according to the determined working temperature setting value. Since the working temperature of the laser is allowed to be changed along with the ambient temperature within a given temperature range, the heating or refrigerating power consumption can be reduced; and moreover, the optical power is previously calibrated to the appropriate range, so that the optical power can still meet the requirement within the variation range of the working temperature of the laser, the bias current is unnecessary to compensate, and the compensation power consumption can be further saved.

The invention discloses a method for analyzing influences of a background ionosphere on GEO SAR imaging. The method includes the steps that a GEO SAR echo signal model influenced by a time-varying ionosphere is established, image offset and defocusing phase which are used for analyzing influences on imaging are derived on the basis of the model, and then judgment of the influences on imaging is performed; during analysis, GEO SAR echo signals influenced by the time-varying ionosphere and the measuring data of the ionosphere total electron content TEC on the propagation paths of the GEO SAR signals are obtained, polynomial fitting is performed on the TEC measuring data three times, a constant term and coefficients of first three items are obtained, echo signal parameters and TEC coefficients are substituted into a derived expression of the image offset and the defocusing phase, and compared with a threshold value, the influences of the background ionosphere on GEO SAR imaging are obtained. According to the method, modeling is performed specifically and is accurate, and imaging analysis is performed on the basis of the accurate model so that the analysis accuracy can be improved.

A method, system, apparatus, and computer program product provide the ability to analyze ionospheric slant total electron content (TEC) using global navigation satellite systems (GNSS)-based estimation. Slant TEC is estimated for a given set of raypath geometries by fitting historical GNSS data to a specified delay model. The accuracy of the specified delay model is estimated by computing delay estimate residuals and plotting a behavior of the delay estimate residuals. An ionospheric threat model is computed based on the specified delay model. Ionospheric grid delays (IGDs) and grid ionospheric vertical errors (GIVEs) are computed based on the ionospheric threat model.

The invention relates to an ionized layer chromatography method and system based on multi-constellation GNSSs. The ionized layer chromatography method comprises the steps that multiple satellite navigation systems are adopted to carry out the ionized layer chromatography, firstly, an object region range is determined, observation data corresponding to all the satellite navigation systems within the object region range are selected; then total electron content corresponding to all the satellite navigation systems is calculated, and the relation between the total electron content of the satellite navigation systems and desired ionized layer electron density is obtained; and finally, the relation between the total electron content of the satellite navigation systems and the desired ionized layer electron density is subjected to inversion calculation, and the ionized layer electron density of the object region range is obtained by the calculation. The ionized layer chromatography operationis carried out through multiple different satellite navigation systems, and compared with an existing operation which is carried out only through one kind of satellite navigation systems, the accuracy of the ionized layer electron density obtained by the inversion is improved greatly, and the reliability of the ionized layer chromatography method is improved equally.

The invention discloses a detection method of real-time GPS (Global Position System) carrier phase cycle slip for frequency taming. The detection method comprises the following steps: S1, calculating an observed value of an MW (Melbourne-Wubbena) wide lane combination, S2, estimating ambiguity of an MW wide lane, S3, calculating a cycle slip decision item, S4, calculating a cycle slip decision threshold, judging whether the cycle slip decision item exceeds the cycle slip decision threshold, and moving to Step S5 if not, S5, calculating an electron content change rate of an ionized layer of an epoch (k), S6, predicting TECR (Total Electron Content Change Rate) value of the epoch (k) according to history data, and S7, calculating a detection threshold of a TECR method, calculating the difference between a calculated value and a predicted value of the epoch (k), and judging whether the detection threshold of the TECR method is exceeded. The method is combined with a constraint condition limitation that the total electron content change rate of the ionized layer is limited in a short period, shows the same cycle slip on L1 and L2 frequency points via linear combination of a carrier phase observation equation, and covers the shortage of an MW method.

The invention discloses a method for calibrating long-wavelength satellite-borne CTLR-mode compact-polarized SAR. The method comprises the following steps of: 1, acquiring an estimated value of an unbalanced error of a receiving channel; 2, acquiring an estimated value of a crosstalk coefficient of a circular-polarized transmitting channel; 3, acquiring an estimated value of a crosstalk coefficient of a linear-polarized receiving channel; 4, acquiring an estimated value of a Faraday rotation angle; and 5, acquiring an unambiguous estimated value of the Faraday rotation angle by using total electron content (TEC) data of a global navigation satellite system (GNSS) to finish SAR calibration. By the method, the processing process is simple and the processing precision is high; and the application of the method in processing of the long-wavelength satellite-borne CTLR-mode compact-polarized SAR data represented by a P wave band is very important.

The invention provides a GNSS base band signal processing method for monitoring the total electron content of the ionized layer. The method for monitoring the TEC of the ionized layer through GNSS double-frequency carrier signals is based on the application characteristics of the GNSS in the field of monitoring the TEC of the ionized layer, addition and subtraction are performed on carrier tracking loop phase discriminators of the GNSS double-frequency signals, and tracking loops of the double-frequency carrier signals are coupled, so that mutual assistance between the double-frequency signal carrier tracking loops is achieved; moreover, code loops are smoothed through differential loop output conversion values of the tracking loops to output the calculated TEC of the ionized layer, and thus the high-precision and high-accuracy value of the TEC of the ionized layer can be obtained. With the GNSS base band signal processing method for monitoring the total electron content of the ionized layer, the precision for monitoring the TECA of the ionized layer can be effectively improved, and effects of cycle slip on the monitored value of the TEC of the ionized layer can be avoided due to the mutual assistance between the double-frequency signals; due to the mutual assistance between the double-frequency signal carrier tracking loops, the double-frequency carrier tracking loops can be assisted mutually by loop tracking information of each other, and thus the tracking sensitivity of the double-frequency signals can be improved.

The invention provides a forecasting method and a device of ionospheric delay of satellite navigation. The method comprises the following steps of: obtaining VTEC (Vertical Total Electron Content) original observation data of ionospheres of global grid points; according to the VTEC original observation data, calculating ionospheric delay of each grid point relative to a navigation signal; and utilizing the calculated ionospheric delay in a former moment to forecast vertical ionospheric delay in a later moment. According to the method, forecast for the ionospheric delay is effectively realized, and a better forecasting effect is obtained. The calculation process is simple and is easily realized, and the method provides a new idea for forecasting the ionospheric delay.

The invention discloses a micro-flow method for measuring total nitrogen content of tobacco. The flow path structure and process parameters of a conventional continuous flow analyzer are modified, including: arranging an air accelerating pipe, changing the inner diameter of a glass coil, changing the inner diameter and flow rate of a pump pipe and adopting a novel reagent preparation method, so that performance optimization is realized, and the using amount of the reagent is saved to the maximum extent. The method runs stably, and the problems of baseline raising, peak pattern drifting and the like do not occur after 60 cups of samples are fed at one time. The micro-flow method has the advantages of high analysis speed (60 samples per hour), high accuracy and high precision, contributes to reduction of reagent consumption, and is suitable for measuring total nitrogen in tobacco and tobacco products on a large scale.

The invention discloses a method for calibrating a compact polarimetric SAR (Synthetic Aperture Radar) in a long wave-length spaceborne pi/4 mode. The method comprises the following steps: 1, acquiring an estimation value of the degree of unbalancedness of a transmission channel; 2, acquiring an estimation value of a channel crosstalk coefficient of a vertical-launching horizontal-receiving component; 3, acquiring an estimation value of a Faraday rotation angle; 4, acquiring an estimation value of an unambiguous Faraday rotation angle by utilizing TEC (Total Electron Content) data provided bya global navigation satellite system; 5, acquiring an estimation value of the degree of unbalancedness of a receiving channel; and 6, acquiring an estimation value of a channel crosstalk coefficient of a horizontal-launching vertical-receiving component. By utilizing the method, accurate calibration still can be performed without scaler errors or system noise, and high-precision calibration can still be performed when the scaler errors and system noise exist. The method provided by the invention has important application value in processing the compact polarimetric SAR data in the long wave-length spaceborne pi/4 mode represented by a P wave band.

The invention discloses an ionized layer error estimation method and an ionized layer error estimation system for a binary offset carrier (BOC) signal. The method comprises the following steps of: tracking pseudo-random noise codes, BOC subcarriers and carrier phases of an intermediate-frequency signal by using a BOC signal tracking ring to obtain a first carrier phase; tracking an upper sidebandsignal of the intermediate-frequency signal to obtain a second carrier phase; tracking a lower sideband signal of the intermediate-frequency signal to obtain a third carrier phase; obtaining a total electron content (TEC) according to the difference between the first carrier phase and the second carrier phase, difference between the first carrier phase and the third carrier phase, the center frequency of a BOC modulating signal, and frequencies of the upper sideband signal and the lower sideband signal; and calculating errors introduced by ionospheric refraction to the carrier phase and pseudorange observation quantity according to the TEC. The BOC signal can be subjected to signal-frequency ionized layer error estimation; and the TEC is calculated by the carrier phases, so the method andthe system are slightly influenced by a multi-path effect and measurement noise.

The invention provides a regional ionospheric TEC (Total Electron Content) real-time monitoring method based on IGS (Internal GNSS Service) and CORSs (Continuously Operating Reference Station), whichcomprises the steps as follows: determining a monitoring region, and dividing the monitoring region into grids according to the size of the monitoring region; determining the longitude and latitude ofeach grid, and determining IGS tracking stations and CORSs participating in establishment of a regional ionospheric grid VTEC (Vertical Total Electron Content) model; reading the data of the IGS tracking stations, the original double-frequency observation data of the CORSs and a navigation message; preprocessing the observation data and the navigation message; calculating the position and elevation angle of a satellite and the longitude and latitude of a puncture point; smoothing a pseudo-range observation value; acquiring the DCB (Difference Code Bias) of the satellite and the DCB of a receiver; extracting the VTEC at the puncture point; carrying out Kriging spatial interpolation and analysis on the puncture point, and broadcasting the result to regional users in a grid form. According to the method, a regional ionospheric grid VTEC model is established by combining IGS and CORS data, the problems of precision reduction and the like caused by insufficiency of the IGS tracking stations are solved, the range of a monitoring region is expanded, and the precision and reliability of the ionospheric grid VTEC model in areas such as the equator are improved.

The invention provides a global ionized layer electron total content prediction method based on a space-time sequence hybrid framework. According to a prediction method, calculation is made on two types of space-time sequences. For a stabilized spatial sequence, an STARMA model prediction method is constructed. For a non-stationary spatio-temporal sequence, the method comprises the following steps: firstly, extracting a nonlinear space-time trend in a non-stationary space-time sequence by adopting a ConvLSTM method; until the extracted residual error passes the stability test; the calculation efficiency can be greatly improved and the calculation time can be saved by using the parallel calculation method, and meanwhile, the global ionospheric electron content distribution characteristicis fully considered, so that the ionospheric prediction algorithm better conforms to the spatial weather law, and the prediction precision is higher.