Generating Vortices with Slowly-growing Gas Giant Planets(2) Then, add a giant planet at r = 1 and...

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Generating Vortices with Slowly-growing Gas Giant Planets Michael Hammer Collaborators: Kaitlin Kratter, Paola Pinilla, Min-Kai Lin University of Arizona van der Marel, N., et al. 2013

Transcript of Generating Vortices with Slowly-growing Gas Giant Planets(2) Then, add a giant planet at r = 1 and...

Page 1: Generating Vortices with Slowly-growing Gas Giant Planets(2) Then, add a giant planet at r = 1 and run the simulation. Gap Two -Fluid (Gas + Dust) Simulations Zhu, Z. et al. 2012 (1b)

Generating Vortices withSlowly-growing Gas Giant Planets

Michael HammerCollaborators: Kaitlin Kratter, Paola Pinilla, Min-Kai Lin

University of Arizona

van der Marel, N., et al. 2013

Page 2: Generating Vortices with Slowly-growing Gas Giant Planets(2) Then, add a giant planet at r = 1 and run the simulation. Gap Two -Fluid (Gas + Dust) Simulations Zhu, Z. et al. 2012 (1b)

Generating Vortices withSlowly-growing Gas Giant Planets

Michael HammerCollaborators: Kaitlin Kratter, Paola Pinilla, Min-Kai Lin

University of Arizona

van der Marel, N., et al. 2013

Page 3: Generating Vortices with Slowly-growing Gas Giant Planets(2) Then, add a giant planet at r = 1 and run the simulation. Gap Two -Fluid (Gas + Dust) Simulations Zhu, Z. et al. 2012 (1b)

Why so asymmetric?

ALMA Observations Hydrodynamic Simulation

Jupiter-mass Planet

SR 21(Dust)

This resemblance is well-known; e.g. (Li, H., et al. 2005; Zhu, Z. + Stone, J. 2014).

Oph IRS 48(Dust)

Perez, L., et al. 2014

Gap

~35 AU

van der Marel, N., et al. 2013

GasHigher Density

Page 4: Generating Vortices with Slowly-growing Gas Giant Planets(2) Then, add a giant planet at r = 1 and run the simulation. Gap Two -Fluid (Gas + Dust) Simulations Zhu, Z. et al. 2012 (1b)

Dust_____

Why so asymmetric?

ALMA Observations Hydrodynamic Simulation

Jupiter-mass Planet

SR 21(Dust)

Oph IRS 48(Dust)

Perez, L., et al. 2014

~35 AU

van der Marel, N., et al. 2013

This resemblance is well-known; e.g. (Li, H., et al. 2005; Zhu, Z. + Stone, J. 2014).

Higher Density

Page 5: Generating Vortices with Slowly-growing Gas Giant Planets(2) Then, add a giant planet at r = 1 and run the simulation. Gap Two -Fluid (Gas + Dust) Simulations Zhu, Z. et al. 2012 (1b)

Why so asymmetric?

ALMA Observations Synthetic Image

Jupiter-mass Planet

SR 21(Dust)

Oph IRS 48(Dust)

Perez, L., et al. 2014

~35 AU

van der Marel, N., et al. 2013

Beam

Higher IntensityThis resemblance is well-known; e.g.

(Li, H., et al. 2005; Zhu, Z. + Stone, J. 2014).

Page 6: Generating Vortices with Slowly-growing Gas Giant Planets(2) Then, add a giant planet at r = 1 and run the simulation. Gap Two -Fluid (Gas + Dust) Simulations Zhu, Z. et al. 2012 (1b)

How can gap-opening planets create vortices?

(1) Start with a gas disk with this radial density profile.To simulate this with FARGO (hydrodynamic code):

Sharp density peaks can make disks unstable(to the RossbyWave Instability)

(2) Then, add a giant planet at r = 1 and run the simulation.

Sharp Peak inRadial Density

Profile

Gap

Page 7: Generating Vortices with Slowly-growing Gas Giant Planets(2) Then, add a giant planet at r = 1 and run the simulation. Gap Two -Fluid (Gas + Dust) Simulations Zhu, Z. et al. 2012 (1b)

Notice:

Vortex Evolution (with Instant Planet Growth)

MH, Kratter, K., Lin, M.-K. 2017, MNRAS, 466, 3533

(1) Extent: The vortex spans 120 degrees near the beginning.

(2) Density: It reaches an over-density of

more than twice the initial density.

(3) Lifetime: It lasts for ~8000 orbits, making

it observable.

Page 8: Generating Vortices with Slowly-growing Gas Giant Planets(2) Then, add a giant planet at r = 1 and run the simulation. Gap Two -Fluid (Gas + Dust) Simulations Zhu, Z. et al. 2012 (1b)

Notice:

(1) Extent: The vortex spans 120 degrees near the beginning.

(2) Density: It reaches an over-density of

more than twice the initial density.

(3) Lifetime: It lasts for ~8000 orbits, making

it observable.

Vortex Evolution (with Instant Planet Growth)

MH, Kratter, K., Lin, M.-K. 2017, MNRAS, 466, 3533

Page 9: Generating Vortices with Slowly-growing Gas Giant Planets(2) Then, add a giant planet at r = 1 and run the simulation. Gap Two -Fluid (Gas + Dust) Simulations Zhu, Z. et al. 2012 (1b)

How fast do giant planets grow?

Core Accretion Model for Giant Planet Formation:Runaway Gas Accretion Phase

Page 10: Generating Vortices with Slowly-growing Gas Giant Planets(2) Then, add a giant planet at r = 1 and run the simulation. Gap Two -Fluid (Gas + Dust) Simulations Zhu, Z. et al. 2012 (1b)

How fast do giant planets grow?

The runaway gas accretion phase can last for thousands of orbits.

Adapted from Lissauer et al. 2009

Growth Models for Jupiter’s Runaway Gas Accretion Phase

Growth Times

Page 11: Generating Vortices with Slowly-growing Gas Giant Planets(2) Then, add a giant planet at r = 1 and run the simulation. Gap Two -Fluid (Gas + Dust) Simulations Zhu, Z. et al. 2012 (1b)

Notice:

(1) Extent: The vortex spans about 240

degrees.

(2) Density: It never reaches double the

initial density.

(3) Lifetime: It lasts for only ~1500 orbits.

Then, it forms a ring.

Vortex Evolution (with Slower Planet Growth)

MH, Kratter, K., Lin, M.-K. 2017, MNRAS, 466, 3533

Page 12: Generating Vortices with Slowly-growing Gas Giant Planets(2) Then, add a giant planet at r = 1 and run the simulation. Gap Two -Fluid (Gas + Dust) Simulations Zhu, Z. et al. 2012 (1b)

Early Vortex Evolution

…with Instant Growth: …with Slower Growth:

(1) Planet grows to full size.

(2) Disk becomes unstable.

(3) A strong vortex forms.

(4) Vortex smooths gap edge.

(1) Disk becomes unstable.

(2) A weak vortex forms.

(3) Vortex smooths gap edge.

(4) Planet grows to full size.

Page 13: Generating Vortices with Slowly-growing Gas Giant Planets(2) Then, add a giant planet at r = 1 and run the simulation. Gap Two -Fluid (Gas + Dust) Simulations Zhu, Z. et al. 2012 (1b)

Vortex Extents with Slower Planet Growth

MH, Kratter, K., Lin, M.-K. 2017, MNRAS, 466, 3533

Concentrated(< 120°)

180 degrees

Page 14: Generating Vortices with Slowly-growing Gas Giant Planets(2) Then, add a giant planet at r = 1 and run the simulation. Gap Two -Fluid (Gas + Dust) Simulations Zhu, Z. et al. 2012 (1b)

Vortex Extents with Slower Planet Growth

MH, Kratter, K., Lin, M.-K. 2017, MNRAS, 466, 3533

Concentrated(< 120°)

180 degrees

Page 15: Generating Vortices with Slowly-growing Gas Giant Planets(2) Then, add a giant planet at r = 1 and run the simulation. Gap Two -Fluid (Gas + Dust) Simulations Zhu, Z. et al. 2012 (1b)

Vortex Extents with Slower Planet Growth

MH, Kratter, K., Lin, M.-K. 2017, MNRAS, 466, 3533

Concentrated(< 120°)

Elongated (> 240°)

180 degrees

Page 16: Generating Vortices with Slowly-growing Gas Giant Planets(2) Then, add a giant planet at r = 1 and run the simulation. Gap Two -Fluid (Gas + Dust) Simulations Zhu, Z. et al. 2012 (1b)

Vortex Extents with Slower Planet Growth

MH, Kratter, K., Lin, M.-K. 2017, MNRAS, 466, 3533

Concentrated(< 120°)

Elongated (> 240°)

180 degrees

Page 17: Generating Vortices with Slowly-growing Gas Giant Planets(2) Then, add a giant planet at r = 1 and run the simulation. Gap Two -Fluid (Gas + Dust) Simulations Zhu, Z. et al. 2012 (1b)

Vortex Extents with Slower Planet Growth

MH, Kratter, K., Lin, M.-K. 2017, MNRAS, 466, 3533

Planets must grow to Jupiter size in <200 orbits

to trigger a concentrated vortex.

Concentrated(< 120°)

Elongated (> 240°)

180 degrees

Page 18: Generating Vortices with Slowly-growing Gas Giant Planets(2) Then, add a giant planet at r = 1 and run the simulation. Gap Two -Fluid (Gas + Dust) Simulations Zhu, Z. et al. 2012 (1b)

Vortex Extents with Slower Planet Growth

MH, Kratter, K., Lin, M.-K. 2017, MNRAS, 466, 3533

No Vortex

Planets must grow to Jupiter size in <200 orbits

to trigger a concentrated vortex.

Typical Jupiter analogsdo not trigger vortices!

(e.g. Lissauer et al. 2009)

Concentrated(< 120°)

Elongated (> 240°)

180 degrees

Page 19: Generating Vortices with Slowly-growing Gas Giant Planets(2) Then, add a giant planet at r = 1 and run the simulation. Gap Two -Fluid (Gas + Dust) Simulations Zhu, Z. et al. 2012 (1b)

Dust Trapping in Vortices?

Gas Dust

Tgrowth = 10 orbits(Concentrated Vortex)

Simulated with Two-Fluid FARGO [Gas + Dust] (Zhu, Z. et al. 2012)MH, Pinilla, P., Kratter, K., Lin, M.-K. 2018, in prep.

Page 20: Generating Vortices with Slowly-growing Gas Giant Planets(2) Then, add a giant planet at r = 1 and run the simulation. Gap Two -Fluid (Gas + Dust) Simulations Zhu, Z. et al. 2012 (1b)

?

Do elongated vortices trap dust the same way?Tgrowth = 1000 orbits

(Elongated Vortex)

Gas DustMH, Pinilla, P., Kratter, K., Lin, M.-K. 2018, in prep.

Simulated with Two-Fluid FARGO [Gas + Dust] (Zhu, Z. et al. 2012)

Page 21: Generating Vortices with Slowly-growing Gas Giant Planets(2) Then, add a giant planet at r = 1 and run the simulation. Gap Two -Fluid (Gas + Dust) Simulations Zhu, Z. et al. 2012 (1b)

Do elongated vortices trap dust the same way?

Concentrated Vortex Elongated Vortex

Contour Levels: 1.10,

Gas1.20, 1.30, 1.40, …, 2.70 [Σ / Σ0]

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Concentrated Vortex

Azimuthal Density Profiles: 1 mm-size grains

MH, Pinilla, P., Kratter, K., Lin, M.-K. 2018, in prep.

Dust

Elongated Vortex

Gaussian (as expected)

Mostly Flat!(not expected!)

Page 23: Generating Vortices with Slowly-growing Gas Giant Planets(2) Then, add a giant planet at r = 1 and run the simulation. Gap Two -Fluid (Gas + Dust) Simulations Zhu, Z. et al. 2012 (1b)

Azimuthal Density Profiles: 1 cm-size grains

MH, Pinilla, P., Kratter, K., Lin, M.-K. 2018, in prep.

Dust

Concentrated Vortex Elongated Vortex

Gaussian (as expected)

Peak is off-center!(not expected!)

Page 24: Generating Vortices with Slowly-growing Gas Giant Planets(2) Then, add a giant planet at r = 1 and run the simulation. Gap Two -Fluid (Gas + Dust) Simulations Zhu, Z. et al. 2012 (1b)

Tgrowth = 1000 orbits(Elongated Vortex)

Why are the elongated vortex peaks off-center?

Planet

The elongated vortex interacts with the

planet’s spiral arms!

MH, Pinilla, P., Kratter, K., Lin, M.-K. 2018, in prep.

Page 25: Generating Vortices with Slowly-growing Gas Giant Planets(2) Then, add a giant planet at r = 1 and run the simulation. Gap Two -Fluid (Gas + Dust) Simulations Zhu, Z. et al. 2012 (1b)

Synthetic Images of Elongated Vortices

Mp = 1 MJupRp = 20 AUTgrowth = 1000 orbits

αdisk = 3 ×10-5

smin = 1 μmsmax = 1 cmn ~ s-3.0

λ = 0.87 mm (Band 7)d = 140 pcBeam: 0.07ʺ × 0.07ʺ

MH, Pinilla, P., Kratter, K., Lin, M.-K. 2018, in prep.

Signature: Peak is off-center in images!

Page 26: Generating Vortices with Slowly-growing Gas Giant Planets(2) Then, add a giant planet at r = 1 and run the simulation. Gap Two -Fluid (Gas + Dust) Simulations Zhu, Z. et al. 2012 (1b)

Resolving the Extent of an Elongated Vortex

Concentrated Vortex Elongated Vortex

A beam diameter of 0.5 rp (0.07ʺ × 0.07ʺ)can resolve the extent and off-center peak of an elongated vortex.

MH, Pinilla, P., Kratter, K., Lin, M.-K. 2018, in prep.

Page 27: Generating Vortices with Slowly-growing Gas Giant Planets(2) Then, add a giant planet at r = 1 and run the simulation. Gap Two -Fluid (Gas + Dust) Simulations Zhu, Z. et al. 2012 (1b)

Resolving the Extent of an Elongated Vortex

Concentrated Vortex Elongated Vortex

A beam diameter of 1.0 rp (0.14ʺ × 0.14ʺ)can resolve the extent and off-center peak of an elongated vortex.

MH, Pinilla, P., Kratter, K., Lin, M.-K. 2018, in prep.

Page 28: Generating Vortices with Slowly-growing Gas Giant Planets(2) Then, add a giant planet at r = 1 and run the simulation. Gap Two -Fluid (Gas + Dust) Simulations Zhu, Z. et al. 2012 (1b)

Resolving the Extent of an Elongated Vortex

Concentrated Vortex Elongated Vortex

A beam diameter of 1.5 rp (0.21ʺ) cannot resolve an elongated vortex.

MH, Pinilla, P., Kratter, K., Lin, M.-K. 2018, in prep.

When observing vortex candiates, request beam sizes of at most the semimajor axis of the planet (not the asymmetry) in your ALMA proposal!

Page 29: Generating Vortices with Slowly-growing Gas Giant Planets(2) Then, add a giant planet at r = 1 and run the simulation. Gap Two -Fluid (Gas + Dust) Simulations Zhu, Z. et al. 2012 (1b)

SummaryJupiter analogs will not trigger vortices unless they

can grow faster than the viscous accretion rate.

If giant planets can still trigger vortices, they would(1) have shorter lifetimes, (2) be less dense,

and (3) be more elongated, making them less likely to observable.

Beam diameters of at most the planet’s semimajor axis are needed to show that a vortex is elongated.

Elongated planet-induced vortices are characterized by (1) wider azimuthal extents and (2) off-center peaks.

Page 30: Generating Vortices with Slowly-growing Gas Giant Planets(2) Then, add a giant planet at r = 1 and run the simulation. Gap Two -Fluid (Gas + Dust) Simulations Zhu, Z. et al. 2012 (1b)

(1) Interpolate from 6 grain sizes to 100 grain sizes from 1 μm to 1 cm.

Generating Synthetic Images

(2) Combine all grain sizes into a single surface density map.

[Grain Size Distribution: n = n0 s-3.0 ]

(4) Convolve simulated images with a beam size.

(3) Run radiative transfer calculations to convertthe density map into a simulated intensity map.

Page 31: Generating Vortices with Slowly-growing Gas Giant Planets(2) Then, add a giant planet at r = 1 and run the simulation. Gap Two -Fluid (Gas + Dust) Simulations Zhu, Z. et al. 2012 (1b)

Do larger grains in elongated vortices still have narrower concentrations? (Yes.)

Page 32: Generating Vortices with Slowly-growing Gas Giant Planets(2) Then, add a giant planet at r = 1 and run the simulation. Gap Two -Fluid (Gas + Dust) Simulations Zhu, Z. et al. 2012 (1b)

Resolving the Extent of an Elongated Vortex

Page 33: Generating Vortices with Slowly-growing Gas Giant Planets(2) Then, add a giant planet at r = 1 and run the simulation. Gap Two -Fluid (Gas + Dust) Simulations Zhu, Z. et al. 2012 (1b)

(1a) Start with a gas disk with the left radial density profile.To simulate this with Two-Fluid FARGO ( ):

(2) Then, add a giant planet at r = 1 and run the simulation.

Gap

Two-Fluid (Gas + Dust) SimulationsZhu, Z. et al. 2012

(1b) Start with a dust disk with same profile, but 100x lower density.

Gap

Particle Sizes: 1 μm, 100 μm, 0.3 mm, 1 mm, 0.3 cm, 1 cm

Page 34: Generating Vortices with Slowly-growing Gas Giant Planets(2) Then, add a giant planet at r = 1 and run the simulation. Gap Two -Fluid (Gas + Dust) Simulations Zhu, Z. et al. 2012 (1b)

Parameter Study

Mass ViscosityPlanet Growth Times

10

(in orbits)

10

10

10

1000

2000

2000

4000

(“Instant”) (Slowest)

Page 35: Generating Vortices with Slowly-growing Gas Giant Planets(2) Then, add a giant planet at r = 1 and run the simulation. Gap Two -Fluid (Gas + Dust) Simulations Zhu, Z. et al. 2012 (1b)

Vortex Lifetimes with Slower Planet Growth

MH, Kratter, K., Lin, M.-K. 2017, MNRAS, 466, 3533

Page 36: Generating Vortices with Slowly-growing Gas Giant Planets(2) Then, add a giant planet at r = 1 and run the simulation. Gap Two -Fluid (Gas + Dust) Simulations Zhu, Z. et al. 2012 (1b)

When are gap edges unstable?

High-Viscosity disks (α >= 3 ×10-3)

will smooth out these peaks.

Low-Viscosity disks (α < 3 ×10-3)

are needed to form vortices.

Not Sharp Enough! Unstable!