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Giant Planet Formation, Evolution, and Internal Structure

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arxiv 1311.1142 v1 pith:QCBLF7E7 submitted 2013-11-05 astro-ph.EP

classification astro-ph.EP
keywords formationgiantmodelsevolutionplanetdifferencesdiskincluding
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The large number of detected giant exoplanets offers the opportunity to improve our understanding of the formation mechanism, evolution, and interior structure of gas giant planets. The two main models for giant planet formation are core accretion and disk instability. There are substantial differences between these formation models, including formation timescale, favorable formation location, ideal disk properties for planetary formation, early evolution, planetary composition, etc. First, we summarize the two models including their substantial differences, advantages, and disadvantages, and suggest how theoretical models should be connected to available (and future) data. We next summarize current knowledge of the internal structures of solar- and extrasolar- giant planets. Finally, we suggest the next steps to be taken in giant planet exploration.

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Cited by 2 Pith papers

Reviewed papers in the Pith corpus that reference this work. Sorted by Pith novelty score. OpenAlex reports about 12 citations worldwide. Full citation record

  1. A Retrieval Framework for Observationally Constraining the Parameters of Circumplanetary Disks

    astro-ph.EP 2026-07 conditional novelty 6.0 of 10

    A calibrated thick-disk semianalytic model plus MCMC retrieval quantifies SED constraints on CPD parameters and recovers consistent masses and accretion rates for PDS 70 b/c and GQ Lup b.

  2. Protoplanetary Disk Survival Time-scales: A Blind Survey of Young Clusters up to 100 Myr in the Solar Vicinity

    astro-ph.SR 2025-07 conditional novelty 6.0 of 10

    Disk fractions in 32 Gaia-selected clusters decline with age at all wavelengths, but the decay is slower at 12 and 22 microns, and long-lived disks are found predominantly around low-mass stars.

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