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Table 2

Same as Table 1, but for different choices of Δσ0.

Δσ0 = 20°–80°

ΔaJ (AU) N4 A4 N5 A5 R45

0.13 143 26–50 106 28–51 1.35
0.14 126 29–52 79 32–53 1.59

Δσ0 = 10°–80°

ΔaJ (AU) N4 A4 N5 A5 R45

0.16 117 20–63 79 29–50 1.48
0.17 106 28–51 63 37–53 1.68

Δσ0 = 0–80°

ΔaJ (AU) N4 A4 N5 A5 R45

0.17 120 29–52 85 30–52 1.41
0.18 94 34–53 60 35–50 1.56

Δσ0 = 0–70°

ΔaJ (AU) N4 A4 N5 A5 R45

0.17 130 30–50 98 30–50 1.33
0.18 99 36–51 66 37–52 1.50

Δσ0 = 0–60°

ΔaJ (AU) N4 A4 N5 A5 R45

0.19 79 36–51 60 36–52 1.32
0.2 67 41–56 41 43–52 1.63

Δσ0 = 0–50°

ΔaJ (AU) N4 A4 N5 A5 R45

0.19 90 39–52 61 40–51 1.47
0.2 71 38–50 46 42–55 1.54

Notes. As long as the migration of Jupiter is fast enough (i.e. ΔaJ is sufficiently large), the L4-to-L5 number ratio R45 can always reach a value of ~1.6, which is capable of explaining the current observation.

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