2016
DOI: 10.1063/1.4965020
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Mathematical model for estimation of meteoroid dark flight trajectory

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Cited by 5 publications
(6 citation statements)
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“…Fireball observations can be also used to infer the individual trajectories of fragments resulting from atmospheric fragmentation. Together with modelling the dark flight, which constitutes the lower part of the trajectory following the termination of the luminous flight, this leads to a con-struction of a strewn field map showing where meteorites could be potentially recovered on the ground [1045,1046].…”
Section: Meteorsmentioning
confidence: 99%
“…Fireball observations can be also used to infer the individual trajectories of fragments resulting from atmospheric fragmentation. Together with modelling the dark flight, which constitutes the lower part of the trajectory following the termination of the luminous flight, this leads to a con-struction of a strewn field map showing where meteorites could be potentially recovered on the ground [1045,1046].…”
Section: Meteorsmentioning
confidence: 99%
“…Furthermore we aim at introducing into the code a build-in recalculation for the realistic atmospheric conditions after Lyytinen & Gritsevich (2016) and see how these could improve the results. We will also calculate the dark-flight trajectory for events identified in the "likely fall" and "possible fall" regions with the algorithms presented in Vinnikov et al (2016), Moilanen et al (2021), andBoaca et al (2021). We plan to apply the algorithm to detections of the FRIPON in other countries.…”
Section: Discussionmentioning
confidence: 99%
“…One can also impose the further condition that the transition from bright to dark-flight must be smooth; most importantly, this means that the rate of change of acceleration should be smooth from bright to dark flight (see Ceplecha 1987). The DFN approach for the core procedure is monotonic; we assume that shape does not change during descent and that there is no fragmentation (see Vinnikov et al 2016). In reality, it is quite possible for fragmentation to occur during the dark flight, as seen in meteorites recovered with broken or missing fusion crust (Folinsbee & Bayrock 1961;Spurný et al 2012).…”
Section: Overviewmentioning
confidence: 99%
“…The shape may also vary during the bright-flight phase owing to ablation or fragmentation, although it is commonly assumed to be fixed during dark flight. (An exception is the dark-flight modeling of Vinnikov et al 2016. ) One approach, as taken by Ceplecha (1987) and similarly used for bright-flight modeling (Ceplecha et al 2000;Revelle 2002;Sansom et al 2015), is to combine these parameters of shape, density, and mass to generate a shape-density parameter (since none of these parameters can be independently constrained from observations) and then use values derived from bright flight as an input to dark-flight modeling.…”
Section: Complicating Factorsmentioning
confidence: 99%
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