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Linearized SDE for Propagating Density Model Uncertainty

机译:用于传播密度模型不确定性的线性化SDE

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Orbital uncertainty or covariance plays an important role in both Space Objects (SO) catalogue maintenance and applications of a SO catalogue. Uncertainty within the estimated orbital elements, initial uncertainty, depends on the method of orbit determination and quality of the observations. The uncertainties in propagated orbital states also depend on the quality of the models employed in representing an orbit and the chosen uncertainty propagation technique. In low Earth orbiters, drag from upper atmosphere is the second most prominent force acting on them, after the perturbing force caused by the oblateness of Earth. Dedicated missions to develop detailed gravity models have reduced uncertainty in gravitational perturbations. The upper atmosphere densities are both spatially and temporally correlated, making it hard to accurately capture within a physical model. The nature of the atmosphere makes it hard to understand the uncertainty within the existing models, and to study its influence on propagating orbital uncertainty. In this paper, we address the problem of covariance propagation due to uncertainty in atmospheric density model. We establish a stochastic model of linear Clohessy-Wiltshire-Hill (CWH) equations of relative motions. The growth of uncertainty in satellite position due to model uncertainty is then obtained by deriving the time variation of covariance of the established Stochastic Differential Equations (SDE). To this end, a simplified exponential model is established, which can be calibrated with real observations. We use it to evaluate the density model induced uncertainties in the propagated states without using an orbit propagator.
机译:orbital不确定性或协方差在空间对象(SO)目录维护和应用程序中起着重要作用。估计轨道元素内的不确定性初始不确定性取决于轨道测定和观察质量的方法。传播的轨道国家的不确定性还取决于代表轨道和所选不确定性传播技术的模型的质量。在低地球轨道轨道中,从上层大气层的拖拽是在由地球左侧引起的扰动力之后作用于它们的第二个最突出的力量。专用任务开发详细的重力模型,在引力扰动中具有降低的不确定性。上大气密度在空间上和时间均相关,使得难以准确地捕获物理模型。大气的性质使其难以理解现有模型内的不确定性,并研究其对传播轨道不确定性的影响。本文在大气密度模型中解决了因不确定性而引起的协方差传播问题。我们建立了相对运动的线性Clohessy-Wiltshire-Hill(CWH)方程的随机模型。然后通过导出建立的随机微分方程(SDE)的协方差的时间变化来获得引起的模型不确定性引起的卫星位置的增长。为此,建立简化的指数模型,可以用真正的观察来校准。我们使用它在不使用轨道传播者的情况下评估传播状态中的密度模型引起的不确定性。

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