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Table 2

Estimates of the mass index s from the existing literature over a meteoroid mass range overlapping to the one observed by Mini-EUSO.

Reference Experiment Technique Mag. range Mass range (kg) Mass index (s)
Hawkins & Upton (1958) HMP Optical [−3, +1] 2.34 ± 0.06
Dohnanyi (1967) HMP Optical [−3, +1] 1.88 ± 0.14
Erickson (1968) HMP Optical [−3, +1] 2.21
Simek & McIntosh (1968) SMO Radar [+5, +10] 2.35 ± 0.10
Thomas et al. (1988) HF radar system Radar 10−10−10−6 2.0 ± 0.1
Cevolani & Gabucci (1996) MFS radar system Radar [−5, +3] 2.07−2.57
Galligan & Baggaley (2004) AMOR Radar 10−10−10−7 2.027 ± 0.006
Blaauw et al. (2011) CMOR Radar >10−8 2.17 ± 0.07
Pokorný & Brown (2016) CMOR Radar 10−8−10−6 2.10 ± 0.08
Pokorný & Brown (2016) CAMO Optical 10−6−10−4 2.08 ± 0.08
Janches et al. (2019) SAAMER Radar 1.98 ± 0.03
Vida et al. (2020) CAMO Optical 10−5−10−3 2.18 ± 0.05
This work Mini-EUSO UV from space [−2, +4.5] 10−5−10−1 2.09 ± 0.02
2.31 ± 0.03

Notes. Columns are (from left to right): bibliographic reference of the study, name or acronym of the experiment, observational technique, magnitude, or mass range of the dataset and mass index (with 1σ uncertainty when provided by the authors). Since not all authors report a direct estimation of the considered mass range of meteoroids, the magnitude range should provide a rough indication of it. However, the reader must be aware that magnitude scales may not be directly comparable with one another (especially when comparing optical and radar measurements). In the case of SAAMER, the authors specify that: “[…] the mass range detected by SAAMER is most likely an overlap between CMOR and AMOR” (Janches et al. 2019). The acronyms of the experiments are: HMP = Harvard Meteor Project, SMO = Springhill Meteor Observatory, HF = high frequency, MFS = meteor forward scatter, AMOR = Advanced Meteor Orbit Radar, CMOR = Canadian Meteor Orbit Radar, CAMO = Canadian Automated Meteor Observatory, SAAMER = Southern Argentina Agile MEteor Radar, and Mini-EUSO for this work.

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