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Geodynamics of Super‐Earth GJ 486b

Abstract:
Many super‐Earths are on very short orbits around their host star and, therefore, more likely to be tidally locked. Because this locking can lead to a strong contrast between the dayside and nightside surface temperatures, these super‐Earths could exhibit mantle convection patterns and tectonics that could differ significantly from those observed in the present‐day solar system. The presence of an atmosphere, however, would allow transport of heat from the dayside toward the nightside and thereby reduce the surface temperature contrast between the two hemispheres. On rocky planets, atmospheric and geodynamic regimes are closely linked, which directly connects the question of atmospheric thickness to the potential interior dynamics of the planet. Here, we study the interior dynamics of super‐Earth GJ 486b ( R = 1.34 $R=1.34$ R ⊕ ${R}_{\oplus }$ , M = 3.0 $M=3.0$ M ⊕ ${M}_{\oplus }$ , T eq ≈ 700 ${\mathrm{T}}_{\text{eq}}\approx 700$ K), which is one of the most suitable M‐dwarf super‐Earth candidates for retaining an atmosphere produced by degassing from the mantle and magma ocean. We investigate how the geodynamic regime of GJ 486b is influenced by different surface temperature contrasts by varying possible atmospheric circulation regimes. We also investigate how the strength of the lithosphere affects the convection pattern. We find that hemispheric tectonics, the surface expression of degree‐1 convection with downwellings forming on one hemisphere and upwelling material rising on the opposite hemisphere, is a consequence of the strong lithosphere rather than surface temperature contrast. Anchored hemispheric tectonics, where downwellings und upwellings have a preferred (day/night) hemisphere, is favored for strong temperature contrasts between the dayside and nightside and higher surface temperatures.
Publication status:
Published
Peer review status:
Peer reviewed

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Publisher copy:
10.1029/2024je008491

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Institution:
University of Oxford
Role:
Author
ORCID:
0000-0003-4143-8482
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Role:
Author
ORCID:
0000-0002-0673-4860
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Role:
Author
ORCID:
0000-0002-3286-7683
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Institution:
University of Oxford
Role:
Author
ORCID:
0000-0002-6893-522X
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Role:
Author
ORCID:
0000-0003-4878-621X


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Funder identifier:
https://ror.org/003x0zc53
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Funder identifier:
https://ror.org/05r0vyz12
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Funder identifier:
https://ror.org/01cmst727
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Funder identifier:
https://ror.org/052csg198


Publisher:
American Geophysical Union
Journal:
Journal of Geophysical Research: Planets More from this journal
Volume:
129
Issue:
10
Article number:
e2024JE008491
Publication date:
2024-10-27
Acceptance date:
2024-09-22
DOI:
EISSN:
2169-9100
ISSN:
2169-9097 and 2169-9100


Language:
English
Keywords:
Source identifiers:
2372633
Deposit date:
2024-10-28
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