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141.
142.
双星导航定位系统采用双星定位体制,其定位基本原理为三球交会测量原理,其中2颗量测量与用户到2颗卫星的距离有关,与用户高程有关的第3个量测量是决定系统定位精度的关键因素.为此,为了简化定位算法,文章根据地球椭球几何及大地纬度的相关知识,推导了与用户高程有关的第3个量测量的精确模型,进而建立了用户的定位算法.该算法具有简单... 相似文献
143.
Nina Zolotukhina Nelya Polekh Olga Pirog 《Advances in Space Research (includes Cospar's Information Bulletin, Space Research Today)》2011
Statistical and spectral analyses are performed to investigate variations of two ionosphere F2 layer key parameters, the critical frequency (foF2) and the peak height (hmF2), that were measured over Irkutsk (52.5°N, 104.0°E) from December 2006 to January 2008 under solar minimum. The analyses showed that both parameters contain quasi-harmonic oscillations with periods of Tn = 24/n hours (n = 1–7), among which the diurnal (n = 1) and semidiurnal (n = 2) ones are the strongest. Seasonal variations are explored of mean and median values, spectrum, amplitude, and phase of the diurnal and semidiurnal components of foF2 and hmF2. 相似文献
144.
M.V. Klimenko V.V. Klimenko K.G. Ratovsky L.P. Goncharenko 《Advances in Space Research (includes Cospar's Information Bulletin, Space Research Today)》2011
In this paper, we use the modified GSM TIP model to explore how the thermosphere–ionosphere system in the American longitudinal sector responded to the series of geomagnetic storms on September 9–14, 2005. Comparison of modeling results with experimental data at Millstone Hill, USA (42.6°N, 71.5°W), Ramey, Puerto Rico (18.3°N, 66.8°W) and Jicamarca, Peru (11.9°S, 76.9°W) has shown a good agreement of ionospheric disturbances in the F-region maximum height. We examine in detail the formation mechanisms of these disturbances at different latitudes and describe some of the important physical processes affecting the behavior of the F-region. In addition, we consider the propagation of thermospheric wind surge and the formation of additional layers in the low-latitude ionosphere during geomagnetic storms. 相似文献
145.
B样条技术在RPM切片数据处理中的应用 总被引:2,自引:0,他引:2
首先介绍了RPM切片数据的处理问题,其次阐述了B样条的基本原理,最后研究了用三次B样条的反求技术对切片数据进行插值修补处理,并用弦高差方法对插值点进行取舍,生成最终的轮廓数据。 相似文献
146.
自旋式飞行器由于运动轨迹复杂,不仅不能精确测量飞行高度,而且从未被用做SAR成像平台。通过研究自旋式飞行器的三维SAR成像新模型,将测高与三维SAR成像相结合,提出了一种基于三维SAR成像的测高新模型。首先分析了自旋式飞行器天线相位中心运动轨迹的特点,将具有三维空间分布的半螺旋线天线运动轨迹等效为面阵天线;然后基于等效面阵,利用模糊函数理论,推导了相应的三维成像模型,从理论上证明了模型的成像可行性并分析其成像性能;最后在成像模型基础上,提出基于三维SAR成像的自旋式飞行器测高新模型,并从成像角度分析影响测高精度的因素。针对等效面阵非均匀分布的特点,采用后向投影(BP)算法仿真验证自旋式飞行器模型下三维成像的可行性和测高模型的有效性。 相似文献
147.
T.L. Gulyaeva P.A. Bradley I. Stanislawska G. Juchnikowski 《Advances in Space Research (includes Cospar's Information Bulletin, Space Research Today)》2008
A numerical model of the peak height of the F2 layer, hmF2_top, is derived from the topside sounding database of 90,000 electron density profiles for a representative set of conditions provided by ISIS1, ISIS2, IK19 and Cosmos-1809 satellites for the period of 1969–1987. The model of regular hmF2 variations is produced in terms of local time, season, geomagnetic latitude, geodetic longitude and solar radio flux. No geomagnetic activity trends were discernible in the topside sounding data. The nighttime peak of hmF2_top evident for mid-latitudes disappears near the geomagnetic equator where a maximum of hmF2_top occurs at sunset hours when it can exceed 500 km at solar maximum. The hmF2 given by the IRI exceeds hmF2_top at the low solar activities. The hmF2_top, obtained by extrapolation of the first derivative of the topside profile to zero shows saturation similar to foF2 the greater the solar activity. The proposed model differs from hmF2 given by IRI based on M(3000)F2 to hmF2 conversion by empirical relationships in terms of foF2, foE and R12 with these quantities mapped globally by the ITU-R (former CCIR) from ground-based ionosonde data. The differences can be attributed to the different techniques of the peak height derivation, different epochs and different global distribution of the source data as well as the different mathematical functions involved in the maps and the model presentation. 相似文献
148.
I. Kutiev P. Marinov A. Belehaki B. Reinisch N. Jakowski 《Advances in Space Research (includes Cospar's Information Bulletin, Space Research Today)》2009
To improve the accuracy of the real time topside electron density profiles given by the Digisonde software a new model-assisted technique is used. This technique uses the Topside Sounder Model (TSM), which provides the plasma scale height (Hs), O+–H+ transition height (HT), and their ratio Rt = Hs/HT, derived from topside sounder data of Alouette and ISIS satellites. The Topside Sounder Model Profiler (TSMP) incorporates TSM and uses the model quantities as anchor points in construction of topside density (Ne) profiles. For any particular location, TSMP calculates topside Ne profiles by specifying the values of foF2 and hmF2. In the present version, TSMP takes the F2 peak characteristics – foF2, hmF2, and the scale height at hmF2 – from the Digisonde measurements. The paper shows results for the Digisonde stations Athens and Juliusruh. It is found that the topside scale height used in Digisonde reconstruction is less than that extracted from topside sounder profiles. Rough comparison of their bulk distributions showed that they differ by an average factor of 1.25 for locations of Athens and Juliusruh. When the Digisonde scale heights are adjusted by this factor, the reconstructed topside profiles are close to those provided by TSM. Compared with CHAMP reconstruction profiles in two cases, TSMP/Digisonde profiles show lower density between 400 and 2000 km. 相似文献
149.
Pencho Marinov Shunrong Zhang Ivan Kutiev 《Advances in Space Research (includes Cospar's Information Bulletin, Space Research Today)》2013
The topside ionosphere scale height extracted from two empirical models are compared in the paper. The Topside Sounder Model (TSM) provides directly the scale height (HT), while the incoherent scatter radar ionospheric model (ISRIM) provides electron density profiles and its scale height (HR) is determined by the lowest gradient in the topside part of the profile. HT and HR are presented for 7 ISR locations along with their dependences on season, local time, solar flux F10.7, and geomagnetic index ap. Comparison reveals that HT values are systematically lower than respective HR values as the average offset for all 7 stations is 55 km. For the midlatitude stations Arecibo, Shigaraki, and Millstone Hill this difference is reduced to 43 km. The range of variations of HR is much larger than that of HT, as the HT range overlaps the lower part of the HR range. Dependences on ap, DoY and LT are much stronger in the ISRIM than in TSM. This results in much larger values of HR at higher ap. Diurnal amplitude of HR is much larger than that of HT, with large maximum of HR at night. The present comparison yields the conclusion that the ISR measurements provide steeper topside Ne profiles than that provided by the topside sounders. 相似文献
150.
The variation of equatorial spread-F occurrences observed by ionosondes at Thailand longitude sector
Sarawoot Rungraengwajiake Pornchai Supnithi Takuya Tsugawa Takashi Maruyama Tsutomu Nagatsuma 《Advances in Space Research (includes Cospar's Information Bulletin, Space Research Today)》2013
The equatorial spread-F (ESF) is a phenomenon of ionopheric irregularities which are mainly generated by the generalized Rayleigh–Taylor (R–T) instability mechanism in conjunction with the other physical mechanisms, originated at the bottom side of the F-layer in the equatorial region after sunset. It degrades the quality of signals that propagate through these irregularities, especially in the navigation satellite system, which requires the high integrity signals. In this work, we analyze the ESF statistics obtained from the FM/CW ionosonde stations over Thailand longitude sector. One is at Chumphon (10.72°N, 99.37°E, dip latitude 3.0°), located near the geomagnetic equator, and the other station is located at Chiangmai (18.76°N, 98.93°E, dip latitude 12.7°). Both stations are as part of the South-East Asia Low Latitude Ionospheric Network (SEALION) project. The ionograms are obtained at every 15 min from September 2004 to August 2005, which has the monthly mean of solar 10.7 cm flux (F10.7) from ∼80 to ∼110. In addition, we compare the diurnal patterns between the ESF occurrences and the variation of virtual height of the F-layer bottom side (h’F) of these two stations. The results show that the ESF occurrences at Chumphon stations are higher than Chiangmai station in all seasons. The high ESF occurrences of both stations mostly occur in equinoctial months corresponded with the rapid rising of the monthly mean h’F in the post-sunset. However, some inconsistent results are still observed, implying the role of other factors such as gravity waves and planetary waves to ESF occurrences. 相似文献