Table 1.
Updated isopoly input parameters (Tp0, riso|p) associated with the isopoly curves accounting for expansion factor modeling in Fig. 6 (two top lines).
Wind type | A | B | C | D | E |
---|---|---|---|---|---|
Tp0 (MK) | 0.65 | 1.1–0.95 | 1.63–1.23 | 2.51–1.56 | 3.71–2.31 |
riso|p (r⊙) | 16.1 | 16.4–16.9 | 13.6–19.9 | 9.2–15.2 | 2.9–8.9 |
T0 (MK) | 0.72 | 0.96–0.88 | 1.17–0.97 | 1.63–1.16 | 2.3–1.6 |
u0 (km/s) | 0.02–1 | 1–6 | 3–10 | 28–18 | 98–42 |
u1 au (km/s) | 292 | 350–370 | 406–416 | 492–527 | 623–645 |
n0 (107 #/cm3) | 3960 | 136–409 | 17–210 | 2–109 | 1–48 |
n1 au (#/cm3) | 10 | 9.7 | 7.2 | 6.2 | 5.4 |
Notes. The estimated mean coronal temperature is shown on the third line. The associated coronal and at 1 au velocities (u0, u1 au), and densities (n0, n1 au), respectively, are shown in the four bottom lines. The initial parameters from Dakeyo et al. (2022) have been modified in order to fit the in situ measured temperatures and velocities of their five wind populations with the computed wind solutions including f(r) modeling. The 1 au density values are also calibrated to the five wind populations in order to have a direct comparison with Dakeyo et al. (2022) isopoly models. Bold values are features of primary interest.
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