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首页> 外文期刊>Journal of geophysical research. Solid earth: JGR >ITRF2005: A new release of the International Terrestrial Reference Frame based on time series of station positions and Earth Orientation Parameters
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ITRF2005: A new release of the International Terrestrial Reference Frame based on time series of station positions and Earth Orientation Parameters

机译:ITRF2005:根据站位置和地球方向参数的时间序列,新发布的国际地面参考系

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Unlike the past International Terrestrial Reference Frame (ITRF) versions where global long-term solutions were combined, the ITRF2005 uses as input data time series (weekly from satellite techniques and 24-h session-wise from Very Long Baseline Interferometry) of station positions and daily Earth Orientation Parameters (EOPs). The advantage of using time series of station positions is that it allows to monitor station non-linear motion and discontinuities and to examine the temporal behavior of the frame physical parameters, namely the origin and the scale. The ITRF2005 origin is defined in such a way that it has zero translations and translation rates with respect to the Earth center of mass, averaged by the Satellite Laser Ranging (SLR) time series spanning 13 years of observations. Its scale is defined by nullifying the scale and its rate with respect to the Very Long Baseline Interferometry (VLBI) time series spanning 26 years of observations. The ITRF2005 orientation (at epoch 2000.0) and its rate are aligned to the ITRF2000 using 70 stations of high geodetic quality. The estimated level of consistency of the ITRF2005 origin (at epoch 2000.0) and its rate with respect to the ITRF2000 is respectively 0.1, 0.8, 5.8 mm and 0.2, 0.1, 1.8 mm/yr along the X, Y and Z-axis. We estimate the formal errors on these components to be 0.3 mm and 0.3 mm/yr. We believe that this low level of agreement between the two frame origins is most probably due to the poor SLR network geometry and its degradation over time. The ITRF2005 combination involving 84 co-location sites revealed a scale inconsistency of 1 ppb (6.3 mm at the equator), at epoch 2000.0, and 0.08 ppb/yr between the SLR and VLBI long-term solutions as obtained by the stacking of their respective time series. Possible causes of this inconsistency may include the poor SLR and VLBI networks and their co-locations, local tie uncertainties, systematic effects and possible inconsistent model corrections used in the data analysis of both techniques. For the first time of the ITRF history, the ITRF2005 rigorous combination provides self-consistent series of EOPs, including Polar Motion from VLBI and satellite techniques and Universal Time and Length of Day from VLBI only. A velocity field of 152 sites with an error less than 1.5 mm/yr is used to estimate absolute rotation poles of 15 tectonic plates that are consistent with the ITRF2005 frame. This new absolute plate motion model supersedes and significantly improves that of the ITRF2000 which involved six major tectonic plates.
机译:与过去的国际地面参考框架(ITRF)版本结合了全球长期解决方案不同,ITRF2005使用站位置和位置的输入数据时间序列(卫星技术每周一次,超长基线干涉法每24小时一次)作为输入数据时间序列。每日地球方向参数(EOP)。使用测站位置的时间序列的优势在于,它可以监视测站的非线性运动和不连续性,并可以检查帧物理参数(即原点和比例尺)的时间行为。 ITRF2005原点的定义方式是,相对于地球质心,其零平移和平移速率为零,这是跨13年观测的卫星激光测距(SLR)时间序列平均得出的。相对于横跨26年观察的超长基线干涉测量(VLBI)时间序列的规模和比率无效,可以定义其规模。 ITRF2005定向(在时代2000.0)及其速率使用70个大地测量质量站与ITRF2000保持一致。沿着X轴,Y轴和Z轴,ITRF2005起点的一致性(在时期2000.0)及其相对于ITRF2000的比率的估计水平分别为0.1、0.8、5.8毫米和0.2、0.1、1.8毫米/年。我们估计这些组件的形式误差为0.3 mm和0.3 mm / yr。我们认为,这两个帧起点之间的协议水平较低,很可能是由于SLR网络的几何形状较差及其随时间而退化的缘故。 ITRF2005组合涉及84个共置位址,表明在2000.0时代的尺度不一致性为1 ppb(赤道为6.3 mm),而SLR和VLBI长期解决方案之间通过堆叠它们各自获得的尺度不一致性时间序列。导致这种不一致的可能原因包括SLR和VLBI网络不佳以及它们的共同位置,局部联系不确定性,系统影响以及两种技术的数据分析中可能使用的不一致的模型校正。 ITRF2005的严格结合是ITRF历史上的第一次,提供了一系列自洽的EOP,包括VLBI的Polar Motion和卫星技术以及VLBI的Universal Time and Day of Day。 152个位置的速度场(误差小于1.5毫米/年)用于估计15个构造板块的绝对旋转极点,这与ITRF2005框架一致。这个新的绝对板块运动模型取代并显着改善了涉及六个主要构造板块的ITRF2000。

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