New Data from Flyby of Pluto

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Image from "The atmosphere of Pluto as observed by New Horizons," by G.R. Gladstone et al. This material relates to a paper that appeared in the March 18, 2016, issue of Science, published by AAAS. The paper, by G.R. Gladstone at Southwest Research Institute in San Antonio, Texas, and colleagues was titled, "The atmosphere of Pluto as observed by New Horizons." Credit: G.R. Gladstone et al. / Science (2016)

Image from “The atmosphere of Pluto as observed by New Horizons,” by G.R. Gladstone et al. This material relates to a paper that appeared in the March 18, 2016, issue of Science, published by AAAS. The paper, by G.R. Gladstone at Southwest Research Institute in San Antonio, Texas, and colleagues was titled, “The atmosphere of Pluto as observed by New Horizons.” Credit: G.R. Gladstone et al. / Science (2016)

Pluto’s surface exhibits a wide variety of landscapes, results from 5 new studies in this special issue on the New Horizons mission report. The dwarf planet has more differences than similarities with its large moon, Charon. What’s more, the studies in this package reveal, Pluto modifies its space environment – interacting with the solar wind plasma and energetic particles around it. The results pave the way for many further, in-depth studies of Pluto.

NASA’s New Horizons mission continues to download information gathered from Pluto and its moon Charon during its historic flyby on 14 July, 2015. Jeffrey Moore et al. offer some of the first descriptions of the wide array of geological features on Pluto and Charon including tectonics, glacial flow, transport of large water-ice blocks, and broad mounds on Pluto – possibly a result of cryovolcanoes.

Data on the variability of terrain suggests the dwarf planet has been frequently resurfaced by processes like erosion, pointing to active geomorphic processes within the last few hundred million years. Such processes have not been active so recently on Charon; divided into a rugged north and a smooth south, the moon is marked with older craters and troughs, contrasting with Pluto.

In a 2nd study, Will Grundy et al. analyze colors and chemical compositions of the icy surfaces of Pluto and Charon. The volatile ices, including water ice and solid nitrogen are distributed in a complicated way due to geomorphic processes acting on the surface over different seasonal and geological timescales. Broad expanses of reddish-brown molecules called tholins accumulated in some parts of Pluto. In a 3rd study, G. Gladstone et al. investigate the atmosphere of Pluto, which is colder and more compact than expected and hosts numerous extensive layers of haze.

In a 4th study, Harold Weaver et al. examine the small moons Styx, Nix, Kerberos, and Hydra, which are irregularly shaped, fast rotating and have bright surfaces. In the 5th, Fran Bagenal et al. report how Pluto modifies its space environment, including interactions with the solar wind and a lack of dust. Taken together, these results from the flyby of Pluto pave the way for scientists’ better understanding of processes of planetary evolution.
http://www.eurekalert.org/pub_releases/2016-03/aaft-fpp031416.php