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Related papers: Pluto's Haze as a Surface Material

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Haze in Pluto's atmosphere was detected in images by both the Long Range Reconnaissance Imager (LORRI) and the Multispectral Visible Imaging Camera (MVIC) on New Horizons. LORRI observed haze up to altitudes of at least 200 km above Pluto's…

Pluto has a heterogeneous surface, despite a global haze deposition rate of ~1 micrometer per orbit (Cheng et al., 2017; Grundy et al., 2018). While there could be spatial variation in the deposition rate, this has not yet been rigorously…

Pluto possesses a thin atmosphere primarily composed of N2, with minor constituents including CO and CH4. Photochemical processes generate distinct haze layers as observed by the New Horizons spacecraft. However, the mechanisms governing…

Pluto, Titan, and Triton make up a unique class of solar system bodies, with icy surfaces and chemically reducing atmospheres rich in organic photochemistry and haze formation. Hazes play important roles in these atmospheres, with physical…

The New Horizons flyby of Pluto confirmed the existence of hazes in its atmosphere. Observations of a large high- to low- phase brightness ratio, combined with the blue color of the haze, suggest that the haze particles are fractal…

The New Horizons spacecraft, which flew by Pluto on July 14, 2015, revealed the presence of haze in Pluto's atmosphere that were formed by CH4/N2 photochemistry at high altitudes in Pluto's atmosphere, as on Titan and Triton. In order to…

Earth and Planetary Astrophysics · Physics 2017-03-08 Tanguy Bertrand , François Forget

One of the many exciting revelations of the New Horizons flyby of Pluto was the observation of global haze layers at altitudes as high as 200 km in the visible wavelengths. This haze is produced in the upper atmosphere through photochemical…

Earth and Planetary Astrophysics · Physics 2023-11-30 Mandt K. E. , Luspay-Kuti A. , Cheng A. , Jessup K. -L. , Gao P

Clouds and hazes are abundant in the thin and cold atmospheres of Triton and Pluto, where they are thought to be produced by interactions between atmospheric gases and ultraviolet photons from the Sun and those scattered by the local…

Earth and Planetary Astrophysics · Physics 2024-11-20 Peter Gao , Kazumasa Ohno

The Pluto system was recently explored by NASA's New Horizons spacecraft, making closest approach on 14 July 2015. Pluto's surface displays diverse landforms, terrain ages, albedos, colors, and composition gradients. Evidence is found for a…

Earth and Planetary Astrophysics · Physics 2021-09-06 S. A. Stern , F. Bagenal , K. Ennico , G. R. Gladstone , W. M. Grundy , W. B. McKinnon , J. M. Moore , C. B. Olkin , J. R. Spencer , H. A. Weaver , L. A. Young , T. Andert , J. Andrews , M. Banks , B. Bauer , J. Bauman , O. S. Barnouin , P. Bedini , K. Beisser , R. A. Beyer , S. Bhaskaran , R. P. Binzel , E. Birath , M. Bird , D. J. Bogan , A. Bowman , V. J. Bray , M. Brozovic , C. Bryan , M. R. Buckley , M. W. Buie , B. J. Buratti , S. S. Bushman , A. Calloway , B. Carcich , A. F. Cheng , S. Conard , C. A. Conrad , J. C. Cook , D. P. Cruikshank , O. S. Custodio , C. M. Dalle Ore , C. Deboy , Z. J. B. Dischner , P. Dumont , A. M. Earle , H. A. Elliott , J. Ercol , C. M. Ernst , T. Finley , S. H. Flanigan , G. Fountain , M. J. Freeze , T. Greathouse , J. L. Green , Y. Guo , M. Hahn , D. P. Hamilton , S. A. Hamilton , J. Hanley , A. Harch , H. M. Hart , C. B. Hersman , A. Hill , M. E. Hill , D. P. Hinson , M. E. Holdridge , M. Horanyi , A. D. Howard , C. J. A. Howett , C. Jackman , R. A. Jacobson , D. E. Jennings , J. A. Kammer , H. K. Kang , D. E. Kaufmann , P. Kollmann , S. M. Krimigis , D. Kusnierkiewicz , T. R. Lauer , J. E. Lee , K. L. Lindstrom , I. R. Linscott , C. M. Lisse , A. W. Lunsford , V. A. Mallder , N. Martin , D. J. McComas , R. L. McNutt , D. Mehoke , T. Mehoke , E. D. Melin , M. Mutchler , D. Nelson , F. Nimmo , J. I. Nunez , A. Ocampo , W. M. Owen , M. Paetzold , B. Page , A. H. Parker , J. W. Parker , F. Pelletier , J. Peterson , N. Pinkine , M. Piquette , S. B. Porter , S. Protopapa , J. Redfern , H. J. Reitsema , D. C. Reuter , J. H. Roberts , S. J. Robbins , G. Rogers , D. Rose , K. Runyon , K. D. Retherford , M. G. Ryschkewitsch , P. Schenk , R. Schindhelm , B. Sepan , M. R. Showalter , K. N. Singer , M. Soluri , D. Stanbridge , A. J. Steffl , D. F. Strobel , T. Stryk , M. E. Summers , J. R. Szalay , M. Tapley , A. Taylor , H. Taylor , H. B. Throop , C. C. C. Tsang , G. L. Tyler , O. M. Umurhan , A. J. Verbiscer , M. H. Versteeg , M. Vincent , R. Webbert , S. Weidner , G. E. Weigle , O. L. White , K. Whittenburg , B. G. Williams , K. Williams , S. Williams , W. W. Woods , A. M. Zangari , E. Zirnstein

Combining findings from New Horizons' suite of instruments reveals a bimodal haze particle distribution within Pluto's atmosphere, which haze models have not been able to reproduce. We employ the photochemical and microphysics KINAERO model…

Earth and Planetary Astrophysics · Physics 2024-02-02 Sihe Chen , Danica Adams , Siteng Fan , Peter Gao , Eliot Young , Yuk Yung

The rotational lightcurves of the Pluto-Charon system were previously believed to be solely attributed to their surfaces. However, a proposed scenario of haze cooling \citep{2017Natur.551..352Z} suggests that the atmospheric haze of Pluto…

Earth and Planetary Astrophysics · Physics 2023-09-20 Linfeng Wan , Xi Zhang , Jason D. Hofgartner

The Alice instrument on NASA's New Horizons spacecraft observed an ultraviolet solar occultation by Pluto's atmosphere on 2015 July 14. The transmission vs. altitude was sensitive to the presence of N2, CH4, C2H2, C2H4, C2H6, and haze. We…

The New Horizons spacecraft mapped colors and infrared spectra across the encounter hemispheres of Pluto and Charon. The volatile ices CH$_4$, CO, and N$_2$, that dominate Pluto's surface, have complicated spatial distributions resulting…

Context. Pluto's tenuous nitrogen (N2) atmosphere undergoes strong seasonal effects due to high obliquity and orbital eccentricity, and has been recently (July 2015) observed by the New Horizons spacecraft. Goals are (i) construct a well…

Earth and Planetary Astrophysics · Physics 2019-05-15 E. Meza , B. Sicardy , M. Assafin , J. L. Ortiz , T. Bertrand , E. Lellouch , J. Desmars , F. Forget , D. Bérard , A. Doressoundiram , J. Lecacheux , J. Marques Oliveira , F. Roques , T. Widemann , F. Colas , F. Vachier , S. Renner , R. Leiva , F. Braga-Ribas , G. Benedetti-Rossi , J. I. B. Camargo , A. Dias-Oliveira , B. Morgado , A. R. Gomes-Júnior , R. Vieira-Martins , R. Behrend , A. Castro Tirado , R. Duffard , N. Morales , P. Santos-Sanz , M. Jelínek , R. Cunniffe , R. Querel , M. Harnisch , R. Jansen , A. Pennell , S. Todd , V. D. Ivanov , C. Opitom , M. Gillon , E. Jehin , J. Manfroid , J. Pollock , D. E. Reichart , J. B. Haislip , K. M. Ivarsen , A. P. LaCluyze , A. Maury , R. Gil-Hutton , V. Dhillon , S. Littlefair , T. Marsh , C. Veillet , K. -L. Bath , W. Beisker , H. -J. Bode , M. Kretlow , D. Herald , D. Gault , S. Kerr , H. Pavlov , O. Faragó , O. Klös , E. Frappa , M. Lavayssière , A. A. Cole , A. B. Giles , J. G. Greenhill , K. M. Hill , M. W. Buie , C. B. Olkin , E. F. Young , L. A. Young , L. H. Wasserman , M. Devogèle , R. G. French , F. B. Bianco , F. Marchis , N. Brosch , S. Kaspi , D. Polishook , I. Manulis , M. Ait Moulay Larbi , Z. Benkhaldoun , A. Daassou , Y. El Azhari , Y. Moulane , J. Broughton , J. Milner , T. Dobosz , G. Bolt , B. Lade , A. Gilmore , P. Kilmartin , W. H. Allen , P. B. Graham , B. Loader , G. McKay , J. Talbot , S. Parker , L. Abe , Ph. Bendjoya , J. -P. Rivet , D. Vernet , L. Di Fabrizio , V. Lorenzi , A. Magazzù , E. Molinari , K. Gazeas , L. Tzouganatos , A. Carbognani , G. Bonnoli , A. Marchini , G. Leto , R. Zanmar Sanchez , L. Mancini , B. Kattentidt , M. Dohrmann , K. Guhl , W. Rothe , K. Walzel , G. Wortmann , A. Eberle , D. Hampf , J. Ohlert , G. Krannich , G. Murawsky , B. Gährken , D. Gloistein , S. Alonso , A. Román , J. -E. Communal , F. Jabet , S. de Visscher , J. Sérot , T. Janik , Z. Moravec , P. Machado , A. Selva , C. Perelló , J. Rovira , M. Conti , R. Papini , F. Salvaggio , A. Noschese , V. Tsamis , K. Tigani , P. Barroy , M. Irzyk , D. Neel , J. P. Godard , D. Lanoiselée , P. Sogorb , D. Vérilhac , M. Bretton , F. Signoret , F. Ciabattari , R. Naves , M. Boutet , J. De Queiroz , P. Lindner , K. Lindner , P. Enskonatus , G. Dangl , T. Tordai , H. Eichler , J. Hattenbach , C. Peterson , L. A. Molnar , R. R. Howell

Numerous solar system atmospheres possess aerosols including the characteristic organic hazes of Titan and Pluto. Haze particles substantially impact atmospheric temperatures structures and may provide organic material to the surface of a…

The New Horizons spacecraft returned images and compositional data showing that terrains on Pluto span a variety of ages, ranging from relatively ancient, heavily cratered areas to very young surfaces with few-to-no impact craters. One of…

On July 14th 2015, NASA's New Horizons mission gave us an unprecedented detailed view of the Pluto system. The complex compositional diversity of Pluto's encounter hemisphere was revealed by the Ralph/LEISA infrared spectrometer on board of…

Pluto's surface is geologically complex because of volatile ices that are mobile on seasonal and longer time scales. Here we analyzed New Horizons LEISA spectral data to globally map the nitrogen ice, including nitrogen with methane diluted…

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