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Wednesday, 4 March 2026

The Orbit of Planet Nine (Part 4)

 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, 9, $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.

  1. CONCLUSION

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)

9

(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)

9

(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)

9

(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)

9

(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 9.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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