Table C.1
Results of the least-square fit on the τ-values in relation to the computed pre-atmospheric velocity ve and pre-atmospheric mass, Me, for different assumed meteoroid densities ρ.
| ρ (kg m−3) | τ − ve relation | τ − Me relation |
|---|---|---|
| 500 |  |
 |
| 1000 |  |
 |
| 1500 |  |
 |
| 2000 |  |
 |
| 2500 |  |
 |
| 3000 |  |
 |
| 3500 |  |
 |
| 4000 |  |
 |
| 4500 |  |
 |
Notes. The results for the weighted least squares method are presented, for which the values are weighted by the relative error of the value. These results are based on the subset investigated by Drolshagen et al. (2021) for the density estimation of ρ = 2500 kg m−3, but six further events were excluded due to the lower and upper boundary for τ. 288 events remain from the 294 evaluated in Drolshagen et al. (2021).
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