the interplay between a hot jupiter's thermal evolution and its atmospheric circulation emily...

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The Interplay Between a Hot Jupiter's Thermal Evolution and its Atmospheric Circulation Emily Rauscher 1,2 Adam Showman 1 1 University of Arizona 2 NASA Sagan Fellow

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Page 1: The Interplay Between a Hot Jupiter's Thermal Evolution and its Atmospheric Circulation Emily Rauscher 1,2 Adam Showman 1 1 University of Arizona 2 NASA

The Interplay Between a Hot Jupiter's Thermal Evolution and its Atmospheric CirculationEmily Rauscher1,2

Adam Showman1

1University of Arizona2NASA Sagan Fellow

Page 2: The Interplay Between a Hot Jupiter's Thermal Evolution and its Atmospheric Circulation Emily Rauscher 1,2 Adam Showman 1 1 University of Arizona 2 NASA

Rauscher

The radiative-convective boundary and the cooling rate

Guillot & Showman (2002)

9/13/11

Arras & Bildsten (2006)

Page 3: The Interplay Between a Hot Jupiter's Thermal Evolution and its Atmospheric Circulation Emily Rauscher 1,2 Adam Showman 1 1 University of Arizona 2 NASA

Rauscher

Downward transport of kinetic energy?

Showman & Guillot (2002)

9/13/11

Efficiency = (downward KE)/(incident flux)

≈ 1%

Page 4: The Interplay Between a Hot Jupiter's Thermal Evolution and its Atmospheric Circulation Emily Rauscher 1,2 Adam Showman 1 1 University of Arizona 2 NASA

Rauscher

Model set-upsame dynamics as Rauscher & Menou 2010, new radiative transfer

9/13/11

Page 5: The Interplay Between a Hot Jupiter's Thermal Evolution and its Atmospheric Circulation Emily Rauscher 1,2 Adam Showman 1 1 University of Arizona 2 NASA

Rauscher

The code9/13/11

Rauscher & Menou, in prep

Double-gray

Page 6: The Interplay Between a Hot Jupiter's Thermal Evolution and its Atmospheric Circulation Emily Rauscher 1,2 Adam Showman 1 1 University of Arizona 2 NASA

Rauscher 9/13/11

The code9/13/11Rauscher

Rauscher & Menou, in prep

Double-gray

Infrared absorption coefficient increases with

pressure

Page 7: The Interplay Between a Hot Jupiter's Thermal Evolution and its Atmospheric Circulation Emily Rauscher 1,2 Adam Showman 1 1 University of Arizona 2 NASA

Rauscher 9/13/11

The code9/13/11Rauscher

Rauscher & Menou, in prep

Double-gray

Infrared absorption coefficient increases with

pressure

At high optical depths transition to diffusion

approximation for radiative flux

Page 8: The Interplay Between a Hot Jupiter's Thermal Evolution and its Atmospheric Circulation Emily Rauscher 1,2 Adam Showman 1 1 University of Arizona 2 NASA

Rauscher 9/13/11

The code Rauscher & Menou, in prep

analytic solution from Guillot (2010),see also Hansen (2008)

Page 9: The Interplay Between a Hot Jupiter's Thermal Evolution and its Atmospheric Circulation Emily Rauscher 1,2 Adam Showman 1 1 University of Arizona 2 NASA

Rauscher

A range of internal heat fluxes

Globally averaged profiles

PRCB at 130, 50, and 20 bar.

9/13/11

Sub- and anti-stellar profiles

Page 10: The Interplay Between a Hot Jupiter's Thermal Evolution and its Atmospheric Circulation Emily Rauscher 1,2 Adam Showman 1 1 University of Arizona 2 NASA

Rauscher

Preliminary results

9/13/11

Page 11: The Interplay Between a Hot Jupiter's Thermal Evolution and its Atmospheric Circulation Emily Rauscher 1,2 Adam Showman 1 1 University of Arizona 2 NASA

Rauscher

Average wind speeds9/13/11

Preliminary

Page 12: The Interplay Between a Hot Jupiter's Thermal Evolution and its Atmospheric Circulation Emily Rauscher 1,2 Adam Showman 1 1 University of Arizona 2 NASA

RauscherZonal wind structure 9/13/11

Tint=125 K Tint=350 K Tint=500 K

Tint=2000 K

Tint=1000 K

Tint=1410 K

Preliminary

Page 13: The Interplay Between a Hot Jupiter's Thermal Evolution and its Atmospheric Circulation Emily Rauscher 1,2 Adam Showman 1 1 University of Arizona 2 NASA

Rauscher

Temperature and wind maps at 1 bar9/13/11

Preliminary

Tint=1000 K

Tint=1410 K

Tint=2000 K

Tint=125 K

Page 14: The Interplay Between a Hot Jupiter's Thermal Evolution and its Atmospheric Circulation Emily Rauscher 1,2 Adam Showman 1 1 University of Arizona 2 NASA

Rauscher

Tint=1000 K

Tint=1410 K

Tint=2000 K

Temperature and wind maps at 150 bar

9/13/11

Tint=500 K

Preliminary

Page 15: The Interplay Between a Hot Jupiter's Thermal Evolution and its Atmospheric Circulation Emily Rauscher 1,2 Adam Showman 1 1 University of Arizona 2 NASA

Rauscher2-D radiative-convective boundary

9/13/11

PRCB,min = 75 bar PRCB,min = 13 bar

PRCB,min = 9 bar

Tint=1000 K

Tint=1410 K

Tint=2000 K

Preliminary

Page 16: The Interplay Between a Hot Jupiter's Thermal Evolution and its Atmospheric Circulation Emily Rauscher 1,2 Adam Showman 1 1 University of Arizona 2 NASA

Rauscher

Efficiency of downward transport of E9/13/11

Preliminary

downward kinetic energyincident stellar heating

=

Page 17: The Interplay Between a Hot Jupiter's Thermal Evolution and its Atmospheric Circulation Emily Rauscher 1,2 Adam Showman 1 1 University of Arizona 2 NASA

Rauscher

Summary

•We see changes in the circulation across a range of internal heat fluxes

•The location of the radiative-convective boundary is 2-D and complex (and requires further analysis)

•The (preliminary) efficiencies we are finding are low, < 0.12%

9/13/11