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Table 1

Best-fit models with no tides (left) and including tides (middle), together with realistic uncertainties of the parameters (right).

var. val. val. Unit σ
m1 1.492735 × 10−12 1.492735 × 10−12 MS 0.16 × 10−12
m2 2 × 10−16 2 × 10−16 MS 2 × 10−16
m3 3 × 10−16 3 × 10−16 MS 3 × 10−16
P1 1.822359 1.822281 day 0.004156
loge1 − 3.991 − 3.991 1 − 3 (i.e. 0.001)
i1 70.104 70.104 deg 1.0
Ω1 252.920 252.920 deg 1.0
ϖ1 0.089 0.089 deg 10.0
λ1 59.665 59.665 deg 1.0
P2 2.745820 2.745791 day 0.004820
loge2 − 3.998 − 3.998 1 − 3
i2 70.347 70.347 deg 1.0
Ω2 252.954 252.954 deg 1.0
ϖ2 1.601 1.601 deg 10.0
λ2 108.357 108.357 deg 1.0
lpole 72.961 72.961 deg 1.0
bpole 19.628 19.628 deg 1.0
Δt1 42.1 s 1.0

nsky 68 68
nsky2 28 28
nao 3240 3240

617 110
66 60
621 621
χ2 872 360

9.07 1.62
2.35 2.14
0.19 0.19

Notes. The left model does not fit the October 10 1980 occultation (see Fig. 1); without this observation, its χ2 would be 368. Orbital elements of the moons are osculating for the epoch T0 = 2454728.761806, where m1 denotes the mass of body 1 (i.e. Kleopatra), m2 body 2 (first moon), m3 body 3 (second moon), P1 the orbital period of the first orbit, e1 eccentricity, i1 inclination, Ω1 longitude of node, ϖ1 longitude of pericentre, λ1 true longitude, etc. of the second orbit; lpole ecliptic longitude of Kleopatra’s rotation pole, bpole ecliptic latitude; n numbers of observations (SKY, SKY2, AO), χ2 values, reduced values. The angular orbital elements are expressed in the standard stellar reference frame. If the orbits lie in the equatorial plane of body 1, they fulfil i = 90° − bpole, Ω = 180° + lpole.

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