Skip to main content

Thermal Processes Governing Hot-Jupiter Radii

Author(s): Spiegel, David S; Burrows, Adam S

Download
To refer to this page use: http://arks.princeton.edu/ark:/88435/pr15h71
Full metadata record
DC FieldValueLanguage
dc.contributor.authorSpiegel, David S-
dc.contributor.authorBurrows, Adam S-
dc.date.accessioned2019-04-10T19:31:00Z-
dc.date.available2019-04-10T19:31:00Z-
dc.date.issued2013-07-20en_US
dc.identifier.citationSpiegel, David S, Burrows, Adam. (2013). Thermal Processes Governing Hot-Jupiter Radii. apj, 772 (76 - 76. doi:10.1088/0004-637X/772/1/76en_US
dc.identifier.urihttp://arks.princeton.edu/ark:/88435/pr15h71-
dc.description.abstractThere have been many proposed explanations for the larger-than-expected radii of some transiting hot Jupiters, including either stellar or orbital energy deposition deep in the atmosphere or deep in the interior. In this paper, we explore the important influences on hot-Jupiter radius evolution of (1) additional heat sources in the high atmosphere, the deep atmosphere, and deep in the convective interior; (2) consistent cooling of the deep interior through the planetary dayside, nightside, and poles; (3) the degree of heat redistribution to the nightside; and (4) the presence of an upper atmosphere absorber inferred to produce anomalously hot upper atmospheres and inversions in some close-in giant planets. In particular, we compare the radius expansion effects of atmospheric and deep-interior heating at the same power levels and derive the power required to achieve a given radius increase when night-side cooling is incorporated. We find that models that include consistent day/night cooling are more similar to isotropically irradiated models when there is more heat redistributed from the dayside to the nightside. In addition, we consider the efficacy of ohmic heating in the atmosphere and/or convective interior in inflating hot Jupiters. Among our conclusions are that (1) the most highly irradiated planets cannot stably have uB 10 km s−1 G over a large fraction of their daysides, where u is the zonal wind speed and B is the dipolar magnetic field strength in the atmosphere, and (2) that ohmic heating cannot in and of itself lead to a runaway in planet radius.en_US
dc.language.isoen_USen_US
dc.relation.ispartofAstrophysical Journalen_US
dc.rightsFinal published version. This is an open access article.en_US
dc.titleThermal Processes Governing Hot-Jupiter Radiien_US
dc.typeJournal Articleen_US
dc.identifier.doidoi:10.1088/0004-637X/772/1/76-
dc.date.eissued2013-07-08en_US
pu.type.symplectichttp://www.symplectic.co.uk/publications/atom-terms/1.0/journal-articleen_US

Files in This Item:
File Description SizeFormat 
Spiegel_2013_ApJ_772_76.pdf912.76 kBAdobe PDFView/Download


Items in OAR@Princeton are protected by copyright, with all rights reserved, unless otherwise indicated.