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METHOD AND SYSTEM FOR NAVIGATION IN REAL TIME USING three carrier radio signal transmitted by satellites, and ionospheric corrections

机译:利用卫星发送的三载波无线电信号进行实时导航和电离层校正的方法和系统

摘要

1.method of navigation in real-time, using three bearing of the first, second and third different frequencies, which u0443u0432u0435u043bu0438u0447u0438u0432u0430u044eu0442u0441u00a0 meaning wu u043au0430u0437u0430u043du043du043eu0439 first to the third frequency, u0434u043bu00a0 u043eu043fu0440u0435u0434u0435u043bu0435u043du0438u00a0 u043fu043eu043bu043eu0436u0435u043du0438u00a0 u043fu043eu043bu044cu0437u043eu0432u0430u0442u0435u043bu00a0, a mobile device, and the signals u043fu0435u0440u0435u0434u0430u044eu0442u0441u00a0 hell, the dunn's m number of transmitters installed on board the artificial satellitesu0434u0432u0438u0436u0443u0449u0438u0445u0441u00a0 in orbit around the earth, and in view of the mobile apparatus, and these signals u043fu0440u0438u043du0438u043cu0430u044eu0442u0441u00a0 receiver u0430u0441u0441u043eu0446u0438u0438u0440u0443u0435u043cu044bu043c the mobile mr apparatus, and receiver u0430u0441u0441u043eu0446u0438u0438u0440u0443u0435u043cu044bu043c with at least one ground station of satellite u0441u0432u00a0u0437u0438 fixed ground stations, called on the u043fu043eu0440u043du044bu043cu0438 u0441u0442u0430u043du0446u0438u00a0u043cu0438, and these signals u043fu0440u043eu0445u043eu0434u00a0u0442 throughthe so-called, u0438u043eu043du043eu0441u0444u0435u0440u043du044bu0439 atmosphere around the earth, and are u0432u043eu0437u043cu0443u0449u0435u043du0438u00a0 that generate phase uncertainty in these bearing frequencies u043eu0442u043bu0438u0447u0430u044eu0449u0438u0439u0441u00a0 in that it includes at least the following stages: the first stage, u0437u0430u043au043bu044eu0447u0430u044eu0449u0438u0439u0441u00a0 in determining the mobile apparatus (sur), the so called of controlled.uncertainty, "especially the phase track" u0440u0430u0437u043du043eu0441u0442u0435u0439 phases between the third and the second the frequency of combinations u043fu0441u0435u0432u0434u043eu0434u0430u043bu044cu043du043eu0441u0442u0435u0439 in the use of a code u0437u043du0430u0447u0435u043du0438u00a0; the second phase, u0437u0430u043au043bu044eu0447u0430u044eu0449u0438u0439u0441u00a0 in the assessment of the mobile apparatus (sur), the so-called"the uncertainty of phase track" u0440u0430u0437u043du043eu0441u0442u0435u0439 phases between the first and second bearing frequencies from the uncertainty, "particularly the u0444u0430u0437u043eu0432 oh, a u0432u0440u0435u043cu00a0 track in the first stage; the third stage, u0437u0430u043au043bu044eu0447u0430u044eu0449u0438u0439u0441u00a0, the mobile apparatus (sur) in the resolution of uncertainty, one of the the frequencies of the uncertainty, "the phase track.u0432u0440u0435u043cu00a0 estimated in the second phase; and an additional stage of u0434u043bu00a0 u043fu0440u0438u043cu0435u043du0435u043du0438u00a0 real-time ionospheric corrections during the u0442u0440u0435u0442u044cu0435u0433 on the stage, and the other ionospheric correction based on continuously u043eu0431u043du043eu0432u043bu00a0u0435u043cu043eu0439 real-time ionospheric model of the u0441u043bu043eu00a0 (u0441ION).;2. method for u043eu0442u043bu0438u0447u0430u044eu0449u0438u0439u0441u00a0 1, so that, in the third phase of the u0432u0440u0435u043cu00a0 permit uncertainty u0432u044bu043fu043eu043bu043du00a0u044eu0442 at the first carrier frequency.;3. method for p.1 or 2, u043eu0442u043bu0438u0447u0430u044eu0449u0438u0439u0441u00a0, u0443u043au0430u0437u0430u043du043du0430u00a0 model u00a0u0432u043bu00a0u0435u0442u0441u00a0 descriptive ionospheric model of the u0438u043eu043du043eu0441u0444u0435u0440u043du043eu0433u043e u0441u043bu043eu00a0 defined on at least one of the uca use of ground reference stations (REF) receiving signals from the specified number of the artificial satellites (SAT1 - GPSE1 - SATn - GPSEn), u0434u0432u0438u0436u0443u0449u0438u0445u0441u00a0 on orbit applications roeg land (gt), and in view of the past.with these signals contain at least two different carrier frequencies, and that the model u043eu043fu0440u0435u0434u0435u043bu00a0u044eu0442 of phase data of the transferring u0430u0435u043cu044bu0445 signals, and the fact that it provides the phase data of the ionosphere model.;4. method for p.3, u043eu0442u043bu0438u0447u0430u044eu0449u0438u0439u0441u00a0 the definition of the model of evaluation u0440u0430u0441u043fu0440u0435u0434u0435u043bu0435u043du0438u00a0 u043eu0441u0443u0449u0435u0441u0442u0432u043bu00a0u044eu0442 ionospheric free electrons in the u0438u043eu043du043eu0441u0444u0435u0440u043du043eu043c layer (u0441ION), and t u0430u043au0436u0435, however, that this assessment u0432u044bu043fu043eu043bu043du00a0u044eu0442 approximately by u0440u0430u0437u0434u0435u043bu0435u043du0438u00a0 u0438u043eu043du043eu0441u0444u0435u0440u043du043eu0433u043e u0441u043bu043eu00a0 (u0441ION) bars of large units (VOxijk) u0440u0430u0437u0440u0435u0448u0435u043du0438u00a0, called "u0432u043eu043au0441u0435u043bu00a0u043cu0438", u043bu0443u0447u0430u0435u043cu0443u044e u0440u0430u0434u0438u043eu0438u0437u043bu0443u0447u0435u043du0438u0435u043c these signalsu0440u0430u0441u043fu0440u043eu0441u0442u0440u0430u043du00a0u044eu0449u0438u0445u0441u00a0 in the u0438u043eu043du043eu0441u0444u0435u0440u043du043eu043c layer (u0441ION), which u0438u043eu043du043eu0441u0444u0435u0440u043du043eu0435 distribution of electronic density in the moment u043fu0440u0435u0434u043fu043eu043bu0430u0433u0430u0435u0442u0441u00a0 u043fu043eu0441u0442u043eu00a0u043du043du044bu043c and that this definition is through permit real-time high electronic density in each of these large units (VOxijk), u043eu0431u043bu0443u0447 u0430u0435u043cu044bu0445 the u0440u0430u0434u0438u043eu0438u0437u043bu0443u0447u0435u043du0438u0435u043c, using the so-calledkalman filter.;5. method for p.4, u043eu0442u043bu0438u0447u0430u044eu0449u0438u0439u0441u00a0 because it provides an additional stage, u0437u0430u043au043bu044eu0447u0430u044eu0449u0438u0439u0441u00a0 operates data u0441u0432u00a0u0437u0430u043du043du044bu0445 the ionospheric model with u0433u0435u043eu0434u0435u0437u0438u0447u0435u0441u043au0438 mi data u0432u044bu0447u0438u0441u043bu00a0u0435u043cu044bu043cu0438 simultaneously, and the fact that the geodetic data u0432u044bu0447u0438u0441u043bu00a0u044eu0442u0441u00a0 only one of these fixed ground reference stations (REFM - r EFME), called the leading station.and u0440u0430u0441u043fu0440u043eu0441u0442u0440u0430u043du00a0u044eu0442u0441u00a0 to the dozens of fixed ground reference stations (REF).;6. method for u043eu0442u043bu0438u0447u0430u044eu0449u0438u0439u0441u00a0 1, so that it provides an additional stage, u0437u0430u043au043bu044eu0447u0430u044eu0449u0438u0439u0441u00a0 using three codes u043fu0441u0435u0432u0434u043eu0434u0430u043bu044cu043du043eu0441u0442u0438, u0441u0432u00a0u0437u0430u043du043du044bu0445 with these three u00a0 with frequencies in the first phase u0432u0440u0435u043cu00a0 u0434u043bu00a0 u043eu043fu0440u0435u0434u0435u043bu0435u043du0438u00a0 so-called uncertainty ", especially the phase track" u0440u0430u0437u043du043eu0441u0442u0435u0439 phases between decree u043du043du044bu043cu0438 third and second bearing frequencies.;7. method for u043eu0442u043bu0438u0447u0430u044eu0449u0438u0439u0441u00a0 2, so that it provides an additional stage, u0437u0430u043au043bu044eu0447u0430u044eu0449u0438u0439u0441u00a0 in performing validation using u043fu0441u0435u0432u0434u043eu0434u0430u043bu044cu043du043eu0441u0442u0438 "the broad phase and code track, and the second code frequency u0434u043bu00a0 u043eu0431u043du0430u0440u0443u0436u0435u043du0438u00a0 jumps, u0441u0432u00a0u0437u0430u043du043du044bu0445 error in the resolution of the uncertainty of the the first frequency.;8.u0441u043fu0443u0442u043du0438u043au043eu0432u0430u00a0 u043du0430u0432u0438u0433u0430u0446u0438u043eu043du043du0430u00a0 system u0434u043bu00a0 realization way on any of the previous paragraphs, u043eu0442u043bu0438u0447u0430u044eu0449u0430u00a0u0441u00a0 because it contains many artificial satellites (s AT1 - GPSE1 - SATn - GPSEn), u0434u0432u0438u0436u0443u0449u0438u0445u0441u00a0 in orbit around the earth (gt), with each of the artificial satellites transmits the signals of three different driving frequencies, at least e, a mobile apparatus (sur)a receiver (SURGPS) of these signals and the computing means which u0432u044bu043fu043eu043bu043du00a0u044eu0442 these first to third stages and integrate these ion u043eu0441u0444u0435u0440u043du044bu0435 correction, ionospheric model derived from the description of the ionosphere, through which radio waves of the passed signals transmitted order u043du043du044bu043c many artificial satellites (SAT1 - GPSE1 - SATn - GPSEn)as well as many fixed ground stations, called u043eu043fu043eu0440u043du044bu043cu0438 u0441u0442u0430u043du0446u0438u00a0u043cu0438 (REF), with u043au0430u0436u0434u0430u00a0 u0441u0442u0430u043du0446u0438u00a0 contains a receiver (REFGPS) accepts the signals from the artificial satellites, the technology u0434u043bu00a0 u043eu043fu0440u0435u0434u0435u043bu0435u043du0438u00a0 the narrative u0438u043eu043du043eu0441u0444u0435u0440u043du043e ionospheric model the u0441u043bu043eu00a0 (u0441ION) and a transmitter (REFE) u0434u043bu00a0 data transmissionof the ionosphere model, to the receiver (SURGPS) mobile apparatus (sur), and, in addition, the fact that at least one of the u0441u0442u0430u0446u0438 u043eu043du0430u0440u043du044bu0445 ground-based reference stations, u043du0430u0437u044bu0432u0430u0435u043cu0430u00a0 leading station (PEFM) includes a receiver (REFMGPS) of the signals transmitted from the multiple artificial travelers (SAT1 - GPSE1 - SATn - GPSEn)the means u0434u043bu00a0 u0432u044bu0447u0438u0441u043bu0435u043du0438u00a0 geodetic data and a transmitter (REFME) u0434u043bu00a0 u0440u0430u0441u043fu0440u043eu0441u0442u0440u0430u043du0435u043du0438u00a0 them by the dozens of fixed ground reference stations (REF).;9. system u043eu0442u043bu0438u0447u0430u044eu0449u0430u00a0u0441u00a0 point 9, so that the mobile apparatus (sur) u043du0430u0445u043eu0434u0438u0442u0441u00a0 on u0440u0430u0441u0441u0442u043eu00a0u043du0438u0438 over 100 km from the nearest fixed ground reference station (REF).
机译:1.实时导航方法,使用第一,第二和第三不同频率的三个方位,其中 u0443 u0432 u0435 u043b u0438 u0447 u0438 u0432 u0430 u044e u0442 u0441 u00a0含义wu u043a u0430 u0437 u0430 u043d u043d u043e u0439第一到第三频率, u0434 u043b u00a0 u043e u043f u0440 u0435 u0434 u0435 u0435 u043b u0435 u043d u0438 u00a0 u043f u043e u043b u043e u0436 u0435 u043d u043b u044b u044c u0437 u043e u0432 u0430 u0442 u0432 u0435 u043b u00b0信号 u043f u0435 u0440 u0435 u0434 u0430 u044e u0442 u0441 u00a0地狱,安装在人造卫星上的dunn的m个发射机数量 u0434 u0432 u0438 u0436 u0443 u0449 u0438 u0445 u0441 u00a0在环绕地球的轨道上,并针对移动设备,并且这些信号 u043f u0440 u0438 u043d u0438 u043c u0430 u044e u0442 u0441 u00a0接收器 u0430 u0441 u0441 u043e u0446 u0438 u0438 u0440 u0443 u0435 u043c u044b u043c移动mr设备我们和接收器 u0430 u0441 u0441 u043e u0446 u0438 u0438 u0440 u0443 u0435 u043c u044b u043c至少具有一个卫星地面站 u0441 u0432 u00a0 u0437 u0438固定地面在 u043f u043e u0440 u043d u044b u043c u0438 u0441 u0442 u0430 u043d u0446 u0438 u00a0 u043c u0438上调用的电台,这些信号 u043f u0440 u043e u0445 u043e u0434 u00a0 u0442,即所谓的 u0438 u043e u043d u043e u0441 u0441 u0444 u0435 u0440 u043d u044b u0439周围的大气层,并且是 u0432 u043e u0437 u043c u0443 u0449 u0435 u043d u0438 u00a0会在这些轴承频率中产生相位不确定性 u043e u0442 u043b u0438 u0447 u0430 u044e u0449 u0438 u0439 u0441 u00a0至少包含接下来的阶段:第一阶段,在确定移动设备(sur)时,即所谓的受控不确定性, “尤其是相位跟踪” u0440 u0430 u0437 u043d u043e u0441 u044 2 u0435 u0439在第三和第二个频率之间的相位是 u043f u0441 u0435 u0432 u0432 u0434 u043e u0434 u0430 u043b u044c u043d u043e u0441 u0441 u0442 u0432 u0435使用代码 u0437 u043d u0430 u0447 u0435 u043d u0438 u00a0;在评估移动设备(sur)时,第二阶段 u0437 u0430 u043a u043b u044e u0447 u0430 u044e u0449 u0438 u0439 u0441 u00a0,即所谓的相位跟踪” u0440 u0430 u0437 u043d u043e u0441 u0442 u0435 u0439相位之间的相位不确定性,尤其是 u0444 u0430 u0437 u043e u0432哦,第一阶段是 u0432 u0440 u0435 u043c u00a0轨道;第三阶段是 u0437 u0430 u043a u043b u044e u0447 u0430 u044e u0449 u0438 u0439 u0441 u00a0在不确定度的分辨率中的设备(sur),不确定度的频率之一,“相位轨迹”。在第二阶段中估计;在 u0442 u0440 u0435 u0442 u044c u0435期间,以及 u0434 u043b u00a0 u043f u0440 u0438 u043c u0435 u043d u0435 u043d u0438 u00a0实时电离层校正的附加阶段 u0433,以及基于连续 u043e u0431 u043d u043e u0432 u043b u00a0 u0435 u043c u043e u0439实时电离层模型的其他电离层校正u00a0( u0441ION);; 2。 u043e u0442 u043b u0438 u0447 u0430 u044e u0449 u0438 u0439 u0441 u00a0 1的方法,因此,在 u0432 u0440 u0435 u0435 u043c u00a0的第三阶段允许不确定性在第一个载波频率上; 3。第1页或第2页的方法, u043e u0442 u043b u0438 u0447 u0430 u044e u0449 u0438 u0439 u0441 u00a0, u0443 u043a u0430 u0437 u0430 u0430 u043d u043d u043d u00a0模型 u00a0 u0432 u043b u00a0 u0435 u0442 u0441 u00a0描述性电离层模型 u0438 u043e u043d u043e u0441 u0444 u0435 u0440 u043d u043e u0433 u043 u043b u043e u00a0定义为从指定数量的人造卫星(SAT1-GPSE1-SATn-GPSEn), u0434 u0432 u0438 u0436 的uca使用地面参考站(REF)中的至少一个鉴于过去,在轨道应用roeg land(gt)上的u0443 u0449 u0438 u0445 u0441 u00a0这些信号至少包含两个不同的载波频率,并且型号 u043e u043f u0440 u0435传输的信号的相位数据的相位数据,并提供电离层模型的相位数据。4 .;第3页的方法, u043e u0442 u043b u0438 u0447 u0430 u044e u0449 u0438 u0439 u0441 u00a0评估模型的定义 u0440 u0430 u0441 u0431 u043f u0440 u0435 u0438 u043e u043中的电离层自由电子u0434 u0435 u043b u0435 u043d u0438 u00a0 u043e u0441 u0443 u0449 u0435 u0431 u0441 u0442 u0432 u043b u0441 u0444 u0435 u0440 u043d u043e u043c图层( u0441ION),而t u0430 u043a u0436 u0435,则此评估 u0432 u044b u043f u043e u043b u043d u00a0 u044e u0442大约是 u0440 u0430 u0437 u0434 u0434 u0435 u043b u0435 u043d u0438 u00a0 u0438 u043e u043d u043e u0441 u0444 u0435 u0440 u043d u043e u043e u0433 u043e u0441 u043b u043e u043e u00a0( u0441ION)条形(VOxijk) u0440 u0430 u0437 u0440 u0435 u0448 u0435 u043d u0438 u00a0,称为“ u0432 u043e u043a u0441 u0435 u043b u00a0 u043c u0438 ”, u043b u0443 u0447 u0430 u0435 u043c u0443 u044e u0440 u0430 u0434 u0438 u043e u0438 u0437 u043b u0443 u0447 u0435 u043d u0438 u0435 u043c这些信号 u0440 u0430 u0430 u044c u043f u0440 u043e u0441 u0442 u0440 u0430 u043d u00a0 u044e u0449 u0438 u0445 u0441 u00a0在 u0438 u043e u043d u043d u043e u0441 u0444 u0435 u04340 u043e u043c层( u0441ION),其中 u043f u0440 u0435 u0434 u043f u043e u043c u043d u043d u043d u043d u043e u0435 u0435 u043e u043b u0430 u0433 u04 30 u0435 u0442 u0441 u00a0 u043f u043e u0441 u0442 u043e u00a0 u043d u043d u044b u043c,并且此定义是通过允许这些大单元中的每个单元实时高电子密度(VOxijk ), u043e u0431 u043b u0443 u0447 u0430 u0435 u043c u044b u0445 u0440 u0430 u04330 u0434 u0438 u043e u0438 u0437 u043437 u043b u0443 u0447 u0435 u043d u043b u0435 u043c,使用所谓的卡尔曼滤波器。; 5。 p.4的方法 u043e u0442 u043b u0438 u0447 u0430 u044e u0449 u0438 u0439 u0441 u00a0,因为它提供了额外的阶段, u0437 u0430 u04330 u043a u043b u043b u044e u0447 u0430 u044e u0449 u0438 u0439 u0441 u00a0运算数据 u0441 u0432 u00a0 u0437 u0430 u043d u043d u043d u044b u0445具有 u0433 u0435 u043e u0434 u0435 u0437的电离层模型u0438 u0447 u0435 u0441 u043a u0438 mi数据 u0432 u044b u0447 u0438 u0441 u043b u00a0 u0435 u043c u044b u043c u0438同时显示,而大地测量数据 u0432 u044b u0447 u0438 u0441 u043b u00a0 u044e u0442 u0441 u00a0只有这些固定地面参考站(REFM-r EFME)中的一个称为引导站。并且 u0440 u0430 u04430 u0441 u043f u0440 将u043e u0441 u0442 u0440 u0430 u043d u00a0 u044e u0442 u0441 u00a0发送到数十个固定地面参考站(REF)。6.。 u043e u0442 u043b u0438 u0447 u0430 u044e u0449 u0438 u0439 u0441 u00a0 1的方法,因此它提供了另一个阶段 u0437 u0430 u043a u043b u043b u044e u0447 u0430 u044e u0449 u0438 u0439 u0441 u00a0使用三个代码 u043f u0441 u0435 u0432 u0434 u043e u0434 u0430 u043b u044c u043d u043e u043e u0441 u0442 u0438, u0441 u043 u00a0 u0437 u0430 u043d u043d u044b u0445,其中的三个 u00a0处于第一相位 u0432 u0440 u0435 u043c u00a0 u0434 u043b u00a0 u043e u043f u0440 u0435 u0434 u0435 u043b u0435 u043d u0438 u00a0所谓的不确定性“,尤其是相位跟踪” u0440 u0430 u0437 u043d u043d u043e u0441 u0442 u0435 u0439在法令 u043d 之间的相位第三和第二轴承频率; 7。 u043e u0442 u043b u0438 u0447 u0430 u044e u0449 u0438 u0439 u0441 u00a0 2的方法,因此它提供了一个附加阶段 u0437 u0430 u043a u043a u043b u043b u044e u0447 u0430 u044e u0449 u0438 u0439 u0441 u00a0使用 u043f u0441 u0435 u0432 u0434 u043e u0434 u0430 u043b u044c u043d u043d u043d u043e u0441 u0442 u0438相位和代码轨,第二个代码频率 u0434 u043b u00a0 u043e u0431 u043d u0430 u0440 u0443 u0436 u0435 u043d u043d u0438 u00a0跳跃, u0441 u0432 u00a0 u0437 u0430 u043d u043d u044b u0445第一频率不确定度的分辨率错误。; 8. u0441 u043f u0443 u0442 u043d u0438 u043a u043e u0432 u0430 u00a0 u043d u0430 u0432 u0438 u0433 u0430 u0446 u0438 u043e u043d u043d u0430 u00a0系统 u0434 u043b u00a0上任一段落的实现方式 u043e u0442 u043b u0438 u0447 u0430 u044e u0449 u0430 u00a0 u0441 u00a0,因为它包含许多人造卫星(s AT1-GPSE1-SATn-GPSEn), u0434 u043 2 u0438 u0436 u0443 u0449 u0438 u0445 u0441 u00a0在环绕地球(gt)的轨道上运行,每个人造卫星都以至少三个e频率发送三个不同驱动频率的信号,即移动设备(sur )这些信号的接收器(SURGPS)和计算装置,这些第一到第三级将这些离子集成到一起。 u0440 u043d u044b u0435修正,是根据电离层描述得出的电离层模型,通过该模型,已通过信号的无线电波按顺序发射了许多人造卫星(SAT1-GPSE1-SATn-GPSEn),以及许多固定地面站,称为 u043e u043f u043e u0440 u043d u044b u043c u0438 u0441 u0442 u0430 u043d u0446 u0438 u00a0 u043c u0438(REF),并带有 u043a u0430 u0436 u0434 u0430 u00a0 u0441 u0442 u0430 u043d u0446 u0438 u00a0包含接收器(REFGPS),用于接收来自人造卫星的信号,技术 u0434 u043b u00a0 u043e u043f u0440 u0435 u0434 u0435 u043b u0435 u043d u0438 u00a0叙事 u0438 u043e u043e u043d u043e u0441 u0444 u043e u043d u043d u043e u0441 u0444 u043d u043e电离层模型 u0441 u043b u043e u00a0( u0441ION)和电离层模型的发射器(REFE) u0434 u043b u00a0数据传输到接收器(SURGPS)移动设备(sur),并且,此外, u0441 u0442 u0430 u0446 u0438 u043e u043d u0430 u0440 u043d u044b u0445地面参考站中至少有一个, u043d u0430 u0430 u0437 u044b u0432 u0430 u0435 u043c u0430 u00a0前端站(PEFM)包括从多个人工旅行者(SAT1- GPSE1- SATn-GPSEn)发射的信号的接收器(REFMGPS),其意思是 u0434 u043b u00a0 u0432 u044b u0447 u0438 u0441 u043b u0435 u043d u0438 u00a0大地测量数据和变送器(REFME) u0434 u043b u00a0 u0440 u0430 u0441 u0431 u043f u0440 u043e u0441 u0442 u042 u04 u0430 u043d u0435 u043d u0438 u00a0由数十个o f固定地面参考站(REF); 9。系统 u043e u0442 u043b u0438 u0447 u0430 u044e u0449 u0430 u00a0 u0441 u00a0点9,因此移动设备(sur) u043d u0430 u0445 u0445 u043e u0434 u0438 u0442 u0440 u0430 u0441 u0441 u0442 u043e u00a0 u043d u0438 u0438上的 u0441 u00a0,距离最近的固定地面参考站(REF)超过100公里。

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