Table 5
Best-fit parameters obtained for the model with the QPC kernel applied to HARPSTERRA and CARMENES-VIS RVs.
Fitted parameter | Best-fit value(a) | |
---|---|---|
eb = 0 | eb ≠ 0 | |
h1,harps (m s−1) | ![]() |
![]() |
h2,harps (m s−1) | 1.4 ± 0.4 | 1.4±0.4 |
h1,CARMENES (m s−1) | 1.1 ± 0.3 | ![]() |
h2,CARMENES (m s−1) | 1.3 ± 0.3 | 1.3±0.3 |
θ (d) | 30.7 ± 0.3 | 30.6±0.3 |
λqpc (d) | ![]() |
![]() |
w | ![]() |
![]() |
γHARPS pre - 2015 (m s−1) | −0.3 ± 0.5 | −0.4±0.5 |
γHARPS post-2015 (m s−1) | 0.0 ± 1.1 | 0.0±1.1 |
γCARMENES (m s−1) | 0.1 ± 0.3 | 0.1±0.3 |
σjit, HARPS pre – 2015 (m s−1) | 0.8 ± 0.1 | 0.7±0.1 |
σjit, HARPS post–2015 (m s−1) | ![]() |
![]() |
σjit,carmenes (m s−1) | 0.9 ± 0.2 | 0.9±0.2 |
Kb (m s−1) | 0.91 ± 0.18 | ![]() |
Pb (d) | ![]() |
140.43±0.41 |
TConj, b (BJD-2450000) | ![]() |
![]() |
![]() |
– | ![]() |
![]() |
– | ![]() |
K365-d,CARMENES (m s−1) | 1.2 ± 0.3 | 1.2±0.3 |
P365-d, CARMENES (d) | ![]() |
![]() |
T0,365-day CARMENES (BJD-2450000) | ![]() |
![]() |
Derived parameter | ||
eccentricity, eb | - | ![]() |
arg. of periapsis, ω*, b | - | ![]() |
min. mass, mb sin ib (M⊕) | 4.7±1.0 | 5.2±0.9 |
semi-major axis, ab (au) | ![]() |
![]() |
periapsis (au) | – | ![]() |
apoapsis (au) | – | ![]() |
equilibrium temperature, Teq, b (K) | 196 ± 10(b) | Orbit-averaged(c): 202±11 |
Apoapsis: ![]() |
||
Periapsis: ![]() |
||
Insolation flux(d), Sb (S⊕) | ![]() |
Orbit-averaged: ![]() |
Apoapsis: ![]() |
||
Periapsis: ![]() |
||
ln Z | −958.0 | −955.2 |
ln Z1p-ln Z0p | +3.3 | +6.1 |
Notes. The model with eb ≠ 0 (values in bold) is our adopted solution. (a)The uncertainties are calculated as the 16th and 84th percentiles of the posterior distributions. (b)Derived from the relation , assuming Bond albedo AB = 0. (c)This is the average equilibrium temperature based on the stellar flux received by the planet averaged over the eccentric orbit. This flux-averaged temperature scales with the eccentricity as
with respect to the value for a circular orbit. (d)For the circular orbit, it is derived from the equation
. For the eccentric orbit, the temporal average insolation flux scales with the eccentricity as
with respect to the value for a circular orbit with the same semi-major axis (e.g. Williams & Pollard 2002).
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