“…More recently, a very simple analytical theory has been developed for flybys of small bodies (Anderson and Giampieri 1999), which also uses the method of variation of parameters, but which adopts unperturbed orbital elements based on the Born approximation for a massless central body. In AG's theory, all gravity terms are treated as perturbations, including the monopole coefficient µ, the product of the gravitational constant by the total mass of the central body.…”
Section: Motivation and Justificationmentioning
confidence: 99%
“…For covariance analyses, these forces are not important since they have no effect on the observable. For trajectory calculations, the rotation perturbations derived by Anderson and Giampieri (1999) can be used to introduce the rotation perturbations into the body-fixed principal axes.…”
“…More recently, a very simple analytical theory has been developed for flybys of small bodies (Anderson and Giampieri 1999), which also uses the method of variation of parameters, but which adopts unperturbed orbital elements based on the Born approximation for a massless central body. In AG's theory, all gravity terms are treated as perturbations, including the monopole coefficient µ, the product of the gravitational constant by the total mass of the central body.…”
Section: Motivation and Justificationmentioning
confidence: 99%
“…For covariance analyses, these forces are not important since they have no effect on the observable. For trajectory calculations, the rotation perturbations derived by Anderson and Giampieri (1999) can be used to introduce the rotation perturbations into the body-fixed principal axes.…”
“…The observable is the range rate , or LOS (line‐of‐sight) Doppler expressed in terms of fractional frequency shift y = Δν/ν, which for purposes of error analysis can be approximated by the first‐order two‐way Doppler formula y = 2/ c , with c the speed of light. The LOS Doppler is obtained by projecting the spacecraft velocity vector along the Earth‐spacecraft direction as follows [ Anderson and Giampieri , 1999]: All quantities in are referred to the closest approach time t = 0, with α and β the direction cosines for the Earth‐spacecraft direction projected, respectively, along the radius and velocity vectors at closest approach. The modulus r of the time‐varying unperturbed radius vector is approximated by .…”
Section: Cometary Mass Determinationmentioning
confidence: 99%
“…The mass parameter GM is designated by μ. The identification of α with the projection along the radius vector and β along the velocity vector is demonstrated by Anderson and Giampieri [1999].…”
[1] Radio Doppler data at X band ($8.4 GHz) and spacecraft attitude control data were obtained during the encounter with comet 81P/Wild 2. The Doppler data set an upper bound of 5 Â 10 15 kg on the mass of the nucleus, about 100 times larger than theoretical estimates. The attitude control data indicate that a large dust particle with a mass in the range of 20 to 40 mg impacted the spacecraft about 15.5 s before closest approach.
“…The vector can be resolved into two components along and across the trajectory direction. In the existing literature (Anderson 1971;Anderson & Giampieri 1999;Rappaport et al 2000) this is accomplished by integration over time with initial conditions at closest approach. Here, we choose to integrate with initial conditions at −∞, which makes a small difference, equal to one-half of the total deflection angle (2), in the direction of the two components.…”
Abstract. During its interplanetary cruise to comet P/Wirtanen, the Rosetta spacecraft will encounter the asteroids 4979 Otawara and 140 Siwa on 11 July 2006 and 24 July 2008, respectively. The objective of the Rosetta Radio Science Investigations (RSI) experiment at these flybys is a determination of the asteroid's mass and bulk density by analyzing the radio tracking data (Doppler and range) received from Rosetta before, during and after closest approach. The spacecraft's flyby trajectory will be gravitationally deflected by an amount proportional to the mass of the asteroid for a given flyby distance and velocity. An analysis of the Doppler noise sources indicates that the mass can be determined to an accuracy of 1% for 140 Siwa. The corresponding bulk density show be accurate to 20%. Unfortunately, a detectable trajectory perturbation seems to be hopeless for Otawara because of its small size and the large nominal flyby distance.
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