March 4, 2026
only from m9 = 5 to m9 = 6 M⊕ and from a9 = 300 to a9 = 310 AU. The orbital angles do not change substantially.
We conclude that the preference for smaller values of mass and semimajor axis is robust, and that the orbital angles (i9, Ω9, $9) are largely unaffected by any contamination. While the posterior distributions for m9 and a9 have large tails towards larger values, the possibility of a closer brighter Planet Nine needs to be seriously considered.
An additional uncertainty worth considering is the diameter and albedo of Planet Nine. We have assumed values appropriate for a gas-rich sub-Neptune which, a priori, seems the most likely state for such a distant body. Given our overall ignorance of the range of possibilities in the outer solar system, we cannot exclude the possibility of an icy body resembling, for ex- ample, a super-Eris. Such an icy/rocky body
could be ∼50% smaller than an equivalent sub- Neptune in this mass range (Lopez & Fortney
2014), and while the large KBOs like Eris have high albedos, much of this elevated albedo could be driven by frost covering of darker irradiated materials as the objects move through very dif- ferent temperature regimes on very eccentric or- bits. An object at the distance of Planet Nine – which stays below the condensation tempera- ture of most volatiles at all times – could well lack such volatile recycling and could have an albedo closer to the ∼10% of the large but not volatile-covered KBOs (Brown 2008). Overall the effect of a smaller diameter and smaller albedo could make Planet Nine ∼ 3 magni- tudes dimmer. Such a situation would make the search for Planet Nine considerably more difficult. While the possibility of a dark super- Eris Planet Nine seems unlikely, it cannot be excluded.
Finally, we recall the affect of the choice of the prior on a9. A prior assuming formation in a cluster would put Planet Nine more distant
than shown here, though it would also predict higher masses. Combining those effects we find that the magnitude distribution seen in Figure 8 would shift fainter by about a magnitude near aphelion but would change little close to peri- helion.
While all of these caveats affect the distance, mass, and brightness of Planet Nine, they have no affect on the sky plane position shown in Figure 8. To a high level of confidence, Planet Nine should be found along this delineated path.
We have presented the first estimate of Planet Nine’s mass and orbital elements using a full statistical treatment of the likelihood of detec- tion of the 11 objects with 150 < a < 1000 AU and q > 42 AU as well as the observa- tional biases associated with these detections. We find that the median expected Planet Nine semimajor axis is significantly closer than previ- ously understood, though the range of potential distances remains large. At its brightest pre- dicted magnitude, Planet Nine could well be in range of the large number of sky surveys being performed with modest telescope, so we expect that the current lack of detection suggests that it is not as the brightest end of the distribution, though few detailed analysis of these surveys has yet been published.
Much of the predicted magnitude range of Planet Nine is within the single-image detec- tion limit of the LSST survey of the Vera Rubin telescope, r ∼ 24.3, though the current survey plan does not extend as far north as the full pre- dicted path of Planet Nine. On the faint end of the distribution, or if Planet Nine is unexpect- edly small and dark, detection will still require
imaging with 10-m class telescopes or larger.
Despite recent discussions, statistical evidence for clustering in the outer solar system remains strong, and a massive planet on a distant in- clined eccentric orbit remains the simplest hy- pothesis. Detection of Planet Nine will usher in a new understanding of the outermost part of our solar system and allow detailed study of a fifth giant planet with mass common through- out the galaxy.
ACKNOWLEDGMENTS
This manuscript owes a substantial debt to the participants at the MATH + X Sympo- sium on Inverse Problems and Deep Learning in Space Exploration held at Rice University in Jan 2019 with whom we discussed the issue of inverting the observations of KBOs to solve for Planet Nine. We would also like to thank two anonymous reviewers of a previous paper whose excellent suggestions ended up being incorpo- rated into this paper and @Snippy X and @si- welwerd on Twitter for advice on notation for our likelihood functions.
Software: HEALPix (Gorski et al. 2005), as- tropy (Astropy Collaboration et al. 2013), scikit- learn (Pedregosa et al. 2011), emcee (Foreman- Mackey et al. 2013), corner (Foreman-Mackey 2016)
Table 2.
-
m9
(Mearth)
a9
(AU)
i9
(deg)
e9
a9
(deg)
Ω9
(deg)
l
∆l
num.
particles
3
625
15
0.60
356
166
-182.1
-9.2
21100
4
230
10
0.15
250
108
-175.5
-2.6
30000
4
250
15
0.15
260
102
-175.3
-2.4
30000
4
500
20
0.33
224
86
-176.2
-3.3
120500
5
230
10
0.15
246
96
-174.3
-1.4
30000
5
250
5
0.15
250
126
-177.0
-4.1
30000
5
250
10
0.15
248
108
-174.4
-1.5
30000
5
260
15
0.10
246
94
-174.2
-1.3
25600
5
260
5
0.15
246
82
-177.0
-4.1
30000
5
280
10
0.10
246
96
-175.8
-2.9
25600
5
280
15
0.10
266
88
-175.0
-2.1
25600
5
300
10
0.15
234
108
-175.6
-2.7
25600
5
300
17
0.15
254
108
-172.9
0.0
25600
5
310
15
0.10
274
102
-175.1
-2.2
25600
5
356
17
0.20
252
88
-174.2
-1.3
25600
5
500
5
0.33
250
96
-179.2
-6.3
25600
5
500
10
0.33
244
86
-176.1
-3.2
25500
5
500
20
0.33
234
86
-176.2
-3.3
20200
5
720
20
0.65
234
96
-185.1
-12.2
30100
6
280
17
0.10
256
100
-173.2
-0.3
25500
6
290
17
0.15
250
108
-173.0
-0.0
25600
6
300
17
0.15
246
100
-173.4
-0.4
25600
6
310
10
0.10
252
96
-174.4
-1.5
25600
6
310
15
0.10
256
96
-174.6
-1.7
25600
6
310
17
0.10
244
108
-175.0
-2.1
25600
6
310
10
0.15
256
108
-173.0
-0.1
25600
6
310
15
0.15
252
116
-173.0
-0.1
25600
6
310
17
0.15
266
106
-173.5
-0.6
19900
6
310
5
0.20
244
108
-177.1
-4.2
25600
6
310
10
0.20
244
108
-173.9
-1.0
25000
6
310
15
0.20
252
92
-173.0
-0.0
25400
Table 2 continued
-
m9
(Mearth)
a9
(AU)
i9
(deg)
e9
a9
(deg)
Ω9
(deg)
l
∆l
num.
particles
6
310
17
0.20
260
122
-173.2
-0.3
13600
6
310
20
0.20
242
96
-173.2
-0.3
23700
6
310
25
0.20
230
92
-174.7
-1.8
20000
6
310
30
0.20
238
88
-178.0
-5.1
25500
6
330
10
0.20
248
108
-174.6
-1.7
31300
6
330
15
0.20
252
92
-173.4
-0.5
14400
6
356
20
0.10
254
100
-175.3
-2.4
25600
6
356
20
0.15
250
110
-174.2
-1.3
25600
6
356
15
0.20
256
102
-174.1
-1.2
21200
6
356
17
0.20
262
100
-174.1
-1.2
25600
6
356
17
0.20
264
108
-173.9
-1.0
25600
6
356
19
0.20
238
100
-173.9
-1.0
48500
6
356
25
0.20
228
88
-176.2
-3.3
40200
6
356
30
0.20
238
96
-179.9
-6.9
16700
6
380
17
0.20
242
110
-174.1
-1.2
25600
6
380
17
0.25
246
92
-173.3
-0.3
25600
6
500
35
0.15
242
96
-181.8
-8.9
30000
6
600
40
0.15
260
94
-184.0
-11.1
30000
6
800
50
0.15
242
82
-188.4
-15.5
30000
7
356
17
0.20
246
92
-173.8
-0.9
25600
7
400
15
0.25
254
82
-173.9
-1.0
30900
7
400
20
0.25
246
102
-175.2
-2.3
52800
7
400
30
0.25
230
88
-177.5
-4.6
30800
7
450
25
0.15
248
108
-178.7
-5.8
30000
7
450
15
0.33
250
86
-175.8
-2.8
29700
7
450
20
0.33
236
80
-175.9
-3.0
25600
7
450
25
0.33
236
80
-176.2
-3.3
23500
7
500
20
0.15
256
94
-176.3
-3.4
25600
7
500
15
0.20
256
102
-175.6
-2.7
25600
7
500
17
0.20
268
96
-175.1
-2.1
25600
7
500
25
0.20
254
92
-177.6
-4.7
25600
7
500
20
0.25
260
94
-176.8
-3.9
25600
7
500
5
0.33
242
96
-178.2
-5.2
57300
Table 2 continued
Table 2 (continued)
-
m9
(Mearth)
a9
(AU)
i9
(deg)
e9
a9
(deg)
Ω9
(deg)
l
∆l
num.
particles
7
500
10
0.33
252
92
-176.6
-3.7
41400
7
500
15
0.33
250
98
-175.5
-2.6
47700
7
500
17
0.33
250
100
-175.4
-2.5
17500
7
500
20
0.33
242
86
-176.1
-3.2
52400
7
500
25
0.33
234
86
-177.9
-5.0
54000
7
500
30
0.33
232
94
-179.0
-6.1
59600
7
500
35
0.33
230
86
-180.5
-7.6
41700
7
500
25
0.40
228
86
-179.7
-6.8
35000
7
500
25
0.45
226
74
-182.0
-9.0
27700
7
525
20
0.50
236
70
-179.6
-6.6
33000
7
550
17
0.40
244
88
-175.6
-2.6
25600
7
600
17
0.45
238
94
-174.9
-2.0
25600
7
640
17
0.50
240
102
-176.8
-3.9
16900
7
650
17
0.45
230
88
-174.6
-1.7
25500
7
800
50
0.15
310
50
-190.4
-17.5
30000
7
830
20
0.70
208
96
-184.7
-11.7
51200
7
1000
60
0.15
298
94
-191.2
-18.3
30000
8
400
20
0.15
248
108
-177.1
-4.2
30000
10
350
10
0.15
250
96
-176.3
-3.4
30000
10
400
20
0.15
242
84
-178.2
-5.3
30000
10
450
20
0.33
242
82
-177.8
-4.9
34300
10
525
20
0.15
264
106
-178.1
-5.2
30000
10
525
30
0.15
266
102
-184.6
-11.7
30000
10
525
40
0.15
304
138
-189.9
-17.0
30000
10
525
20
0.50
244
114
-180.8
-7.9
39700
10
525
20
0.65
242
90
-181.7
-8.8
20900
10
525
30
0.65
244
36
-187.1
-14.2
35600
10
700
20
0.35
244
108
-176.6
-3.7
25600
10
700
30
0.70
290
132
-190.0
-17.1
25600
10
750
10
0.35
234
106
-177.5
-4.6
19500
10
750
15
0.35
252
114
-176.1
-3.2
22400
10
750
20
0.35
244
100
-177.9
-5.0
25500
10
800
5
0.40
244
114
-177.5
-4.6
25600
Table 2 continued
-
m9
(Mearth)
a9
(AU)
i9
(deg)
e9
a9
(deg)
Ω9
(deg)
l
∆l
num.
particles
10
800
10
0.40
240
112
-177.0
-4.1
25600
10
800
15
0.40
240
118
-177.8
-4.9
25600
10
800
15
0.45
240
120
-174.9
-2.0
25600
10
800
20
0.45
238
108
-176.0
-3.1
28600
10
800
25
0.45
234
100
-177.6
-4.7
23500
10
800
30
0.45
242
50
-184.0
-11.1
16800
10
800
60
0.45
182
114
-183.0
-10.1
30400
10
870
20
0.73
254
92
-185.4
-12.5
17900
10
1000
60
0.15
314
96
-192.8
-19.9
23600
10
1400
70
0.15
224
30
-190.0
-17.1
30000
12
500
15
0.20
256
94
-178.4
-5.5
25600
12
500
20
0.20
256
92
-181.2
-8.3
25600
12
500
25
0.20
266
102
-182.9
-10.0
25600
12
920
20
0.73
224
76
-182.1
-9.1
25800
12
960
20
0.79
242
54
-186.8
-13.9
24900
14
960
20
0.74
220
76
-185.6
-12.7
28000
16
1000
20
0.75
248
76
-183.2
-10.2
33600
20
900
60
0.15
306
66
-189.0
-16.1
30000
20
1000
15
0.65
242
122
-179.6
-6.7
30100
20
1000
20
0.65
240
118
-180.6
-7.7
33000
20
1000
25
0.65
246
70
-185.5
-12.6
32300
20
1070
20
0.77
240
124
-185.2
-12.3
64900
20
1400
70
0.15
264
0
-186.8
-13.9
30000
20
2000
80
0.15
260
152
-190.1
-17.2
30000
Note—Parameters used in the numerical simulations on the effects of Planet Nine (m9, a9, i9, e9) and the maximum ln(likelihood), l, which occurs at the listed value of a9 and Ω9. ∆l gives the difference in ln(likelihood) from the maximum value, which occurs at m9 = 5, a9 = 310, i9 = 15, and e9 = 0.10.
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