共查询到18条相似文献,搜索用时 125 毫秒
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针对蒸发波导高度在海洋上水平分布不均匀,进而影响雷达探测距离的问题,采用雷达探测距离评估模式,对蒸发波导高度随距离变化条件下雷达探测距离进行仿真分析,结果表明当雷达天线位于水平非均匀的蒸发波导内,雷达在蒸发波导低的一侧向蒸发波导高的一侧探测时,雷达最大作用距离超过蒸发波导高的一侧向蒸发波导低的一侧探测时雷达的最大作用距离,这与视蒸发波导高度为水平均匀的采用单站蒸发波导数据评估雷达最大探测距离的结论相反。说明在蒸发波导高度水平分布非均匀的海域评估雷达作用距离时,需要获取大于雷达作用距离的蒸发波导数据,采用随距离变化的蒸发波导评估雷达作用距离。 相似文献
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《中国海洋大学学报(自然科学版)》2017,(2)
高频地波雷达对海上目标跟踪探测时,由于距离和方位角分辨率低且受到随机噪声的干扰,导致对目标位置探测不准确,形成的航迹会偏离目标的真实位置,影响跟踪的准确性。针对这个问题,结合海上特定目标跟踪的实际,本文从航迹的角度出发,基于对距离和方位角误差时间序列的统计建模,提出了一种基于同步船舶自动识别系统(Automatic Identification System,AIS)信息的高频地波雷达海上目标航迹校正方法。在高频地波雷达与AIS同步跟踪期间,采用统计回归的方法建立目标距离和方位角误差的校正模型;在高频地波雷达独立跟踪时,利用得到的模型分别对距离和方位角进行校正。利用实测高频地波雷达目标探测数据进行了航迹校正实验,校正后距离和方位角的均方根误差分别减少了约90%和75%,航迹跟踪效果得到了显著改善。 相似文献
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高频地波雷达是海上目标大范围连续跟踪探测的有效手段,在其探测结果中,目标的距离是一个重要的参数,其探测精度会影响目标的整体探测性能。本文给出了地波雷达目标距离参数的估计方法和处理流程,并基于地波雷达实测数据开展了目标距离估计及距离-速度耦合补偿处理,将目标距离参数估计结果与实测船舶自动识别系统数据开展了比对,统计分析了目标距离参数在补偿处理前后的误差及其影响因素。结果表明,目标距离参数经过耦合补偿处理之后,测距误差明显减小,测距精度得到了显著提高,最后结合个例分析,给出了距离补偿大小和正负与目标航向的关系。 相似文献
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海上作战一旦遇到大气波导,可使船载电子信息系统之间的短波通信距离增大数倍,同时通信距离范围内的部分区域会出现电磁盲区。该文以海上战场环境为背景,阐述了海上大气波导对未来海上作战的重要性。通过对大气波导的形成机制和影响机理进行研究,系统化概括了蒸发波导、表面波导和抬升波导的观测原理及常用观测方法。通过对比分析传统大气波导的观测方法,发现其在观测手段、观测精度、观测范围和观测成本方面存在局限性。基于此,该文提出一种多物理场协同探测的大气波导观测方法,该方法通过集合海上浮标网、船联网、星联网和岸基网等各类观测仪器和设备,可实时获取海上大气参数,构建海上大气波导预报系统。最终,通过该预报系统可实现海上大气波导大范围、高精度、实时性预报,对海上作战掌握制空权具有重要意义。 相似文献
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A new method for estimating high-frequency radar error using data from Central San Francisco Bay 总被引:1,自引:0,他引:1
Maxwell Hubbard Donald Barrick Newell Garfield Jim Pettigrew Carter Ohlmann Matthew Gough 《Ocean Science Journal》2013,48(1):105-116
This study offers a new method for estimating High-Frequency (HF) radar surface current velocity error in data comparisons with other types of instrumentation. A new method is needed in order to remove the zero-mean random spatial and temporal fluctuations present in surface-current measurements from all sensors. Conventional methods for calculating radar error when comparing with another instrument have included their root mean square differences and scatter plots that provide correlation coefficient and slope/intercept of the regression line. It seems that a meaningful estimate of radar error should attempt to remove both sensors’ zero mean random fluctuations, inasmuch as possible. We offer and compare a method that does this. The method was tested on data collected in the Central San Francisco Bay, where GPS surface-drifter deployments were conducted within the coverage of four 42 MHz radars over six days in October of 2008. Drifters were continuously deployed in these areas over the sampling days, providing 525 usable drifter measurements. Drifter and radar measurements were averaged into thirty-minute time bins. The three-day long-term averages from the sampling areas were then subtracted from the thirtyminute averages to remove biases associated with comparisons done with short, disjoint time-sample periods. These were then used to develop methods that give radar error or bias after the random fluctuations have been removed. Results for error estimates in this study are commensurate with others where random fluctuations have been filtered, suggesting they are valid. The estimated error for the radars in the SF Bay is low, ranging from ?7.57 cm/s to 0.59 cm/s. 相似文献
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The 1-Centimeter Orbit: Jason-1 Precision Orbit Determination Using GPS, SLR, DORIS, and Altimeter Data 总被引:1,自引:0,他引:1
S. B. Luthcke N. P. Zelensky D. D. Rowlands F. G. Lemoine T. A. Williams 《Marine Geodesy》2003,26(3):399-421
The Jason-1 radar altimeter satellite, launched on December 7, 2001 is the follow on to the highly successful TOPEX/Poseidon (T/P) mission and will continue the time series of centimeter level ocean topography measurements. Orbit error is a major component in the overall error budget of all altimeter satellite missions. Jason-1 is no exception and has set a 1-cm radial orbit accuracy goal, which represents a factor of two improvement over what is currently being achieved for T/P. The challenge to precision orbit determination (POD) is both achieving the 1-cm radial orbit accuracy and evaluating the performance of the 1-cm orbit. There is reason to hope such an improvement is possible. The early years of T/P showed that GPS tracking data collected by an on-board receiver holds great promise for precise orbit determination. In the years following the T/P launch there have been several enhancements to GPS, improving its POD capability. In addition, Jason-1 carries aboard an enhanced GPS receiver and significantly improved SLR and DORIS tracking systems along with the altimeter itself. In this article we demonstrate the 1-cm radial orbit accuracy goal has been achieved using GPS data alone in a reduced dynamic solution. It is also shown that adding SLR data to the GPS-based solutions improves the orbits even further. In order to assess the performance of these orbits it is necessary to process all of the available tracking data (GPS, SLR, DORIS, and altimeter crossover differences) as either dependent or independent of the orbit solutions. It was also necessary to compute orbit solutions using various combinations of the four available tracking data in order to independently assess the orbit performance. Towards this end, we have greatly improved orbits determined solely from SLR+DORIS data by applying the reduced dynamic solution strategy. In addition, we have computed reduced dynamic orbits based on SLR, DORIS, and crossover data that are a significant improvement over the SLR- and DORIS-based dynamic solutions. These solutions provide the best performing orbits for independent validation of the GPS-based reduced dynamic orbits. The application of the 1-cm orbit will significantly improve the resolution of the altimeter measurement, making possible further strides in radar altimeter remote sensing. 相似文献
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《Marine Geodesy》2013,36(3-4):399-421
The Jason-1 radar altimeter satellite, launched on December 7, 2001 is the follow on to the highly successful TOPEX/Poseidon (T/P) mission and will continue the time series of centimeter level ocean topography measurements. Orbit error is a major component in the overall error budget of all altimeter satellite missions. Jason-1 is no exception and has set a 1-cm radial orbit accuracy goal, which represents a factor of two improvement over what is currently being achieved for T/P. The challenge to precision orbit determination (POD) is both achieving the 1-cm radial orbit accuracy and evaluating the performance of the 1-cm orbit. There is reason to hope such an improvement is possible. The early years of T/P showed that GPS tracking data collected by an on-board receiver holds great promise for precise orbit determination. In the years following the T/P launch there have been several enhancements to GPS, improving its POD capability. In addition, Jason-1 carries aboard an enhanced GPS receiver and significantly improved SLR and DORIS tracking systems along with the altimeter itself. In this article we demonstrate the 1-cm radial orbit accuracy goal has been achieved using GPS data alone in a reduced dynamic solution. It is also shown that adding SLR data to the GPS-based solutions improves the orbits even further. In order to assess the performance of these orbits it is necessary to process all of the available tracking data (GPS, SLR, DORIS, and altimeter crossover differences) as either dependent or independent of the orbit solutions. It was also necessary to compute orbit solutions using various combinations of the four available tracking data in order to independently assess the orbit performance. Towards this end, we have greatly improved orbits determined solely from SLR+DORIS data by applying the reduced dynamic solution strategy. In addition, we have computed reduced dynamic orbits based on SLR, DORIS, and crossover data that are a significant improvement over the SLR- and DORIS-based dynamic solutions. These solutions provide the best performing orbits for independent validation of the GPS-based reduced dynamic orbits. The application of the 1-cm orbit will significantly improve the resolution of the altimeter measurement, making possible further strides in radar altimeter remote sensing. 相似文献
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High-frequency (HF) ground wave radar (GWR) is emerging as a significant tool for monitoring ocean surface conditions at ranges well beyond the line-of-sight horizon that limits conventional systems. An experimental GWR system at Cape Race, Newfoundland, Canada that has been operational since 1991, has the ability to performing routine surveillance of oceanic surface parameters and surface target detection. Operating in the frequency range between 5 and 8 MHz, the frequency modulated interrupted continuous wave (FMICW) radar has a nominal range capability of 200 km. An experiment was performed during the period of October 20-November 21, 1992 to test the surface current measuring capability of the Cape Race system. Here, near real-time radial surface current information is extracted from the Doppler spectra of the radar time series data and a comparison is performed to the Lagrangian velocities derived from the position-time tracks of Accurate Surface Tracker (AST) drifters. A wide range of oceanic conditions were experienced during the experimental period, and favorable results were obtained from the comparison regardless of the sea state conditions. The analysis shows the standard deviation in the radar radial velocity component to be approximately 5 cm/s 相似文献
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Among the fastest‐growing applications of high‐precision GPS positioning are those which are kinematic in nature. Carrier phase‐based GPS positioning of a moving antenna—for example, attached to a ship, an aircraft, or a land vehicle—is now commonplace. Recent software innovations make use of advanced ambiguity resolution “on the fly” and real‐time kinematic data processing algorithms to emulate the ease of operation of conventional differential GPS (DGPS) based on transmitted pseudo‐range corrections. However, as much higher accuracy must now be assured compared to DGPS, greater attention must be focused on the quality control aspects of GPS positioning. This study describes two methods for detecting failures or changes of small magnitude in real time in GPS measurements. Examination of the overlap or disjointedness of robust and conventional confidence intervals and studentized normal variates have been used as failure detection tools. These methods are based on testing the performance of the differences between the conventional (nonrobust) Kalman state estimates and the robust Kalman filler estimates. Detection of cycle slips in carrier phase data, outliers in phase rate or in code ranges, or any other type of disorder in the measurements of the GPS system can be addressed with these failure detection methods. Application and evaluation of the algorithms has been carried out using raw carrier‐phase and phase‐rate GPS measurements. It has been demonstrated that these failure detection tools provide powerful and efficient diagnostics for detecting small changes in the measurements of the GPS system. 相似文献
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