Concept art of the evaporating protoplanetary disk. Image:
NASA/JPL-Caltech/T. Pyle (SSC)
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Now, scientists led by Beibei Liu, a physicist at Zhejiang University in China, have proposed a new mechanism that can explain how these giants ended up in their distant orbits, and can even account for some of the puzzling features of the solar system’s innermost rocky worlds, such as Earth and Mars.
A previous hypothesis, known as the Nice model after the French city where it originated, proposed that the orbital instabilities arose after the evaporation of the cloudy primordial disk that birthed our solar system. Now, Liu and his colleagues present results from 14,000 simulations that suggest this evaporating cloud was, itself, the driver of the turbulent effects that led to the familiar planetary configuration we live in today, according to a study published on Wednesday in Nature. Study co-authors Seth Jacobson, a planetary scientist at Michigan State University, and Sean Raymond, an astronomer at the Laboratoire d'Astrophysique de Bordeaux in France, first started developing this new explanation a few years ago.“While the evidence for a giant planet instability in the solar system is clear, both Sean and I knew that there was mounting evidence that the instability must have taken place much earlier than originally hypothesized in the 2005 Nice model,” Jacobson said in an email.
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