2024-03-29T09:01:31Zhttp://digital.csic.es/dspace-oai/requestoai:digital.csic.es:10261/1672462020-12-09T18:01:22Zcom_10261_97com_10261_4col_10261_350
DIGITAL.CSIC
author
Olkin, C.B.
author
Young, L.A.
author
Borncamp, D.
author
Pickles, A.
author
Sicardy, B.
author
Assafin, M.
author
Bianco, F.B.
author
Buie, M.W.
author
De Oliveira, A.D.
author
Gillon, M.
author
French, R.G.
author
Ramos Gomes, A.
author
Jehin, E.
author
Morales, N.
author
Opitom, C.
author
Ortiz, José Luis
author
Maury, A.
author
Norbury, M.
author
Braga-Ribas, F.
author
Smith, R.
author
Wasserman, L.H.
author
Young, E.F.
author
Zacharias, M.
author
Zacharias, N.
funder
National Aeronautics and Space Administration (US)
2018-07-02T07:48:26Z
2018-07-02T07:48:26Z
2015
Icarus 246: 220- 225 (2015)
http://hdl.handle.net/10261/167246
10.1016/j.icarus.2014.03.026
http://dx.doi.org/10.13039/100000104
© 2014 The Authors. Combining stellar occultation observations probing Pluto's atmosphere from 1988 to 2013, and models of energy balance between Pluto's surface and atmosphere, we find the preferred models are consistent with Pluto retaining a collisional atmosphere throughout its 248-year orbit. The occultation results show an increasing atmospheric pressure with time in the current epoch, a trend present only in models with a high thermal inertia and a permanent N<inf>2</inf> ice cap at Pluto's north rotational pole.
eng
openAccess
Occultations
Atmospheres: evolution
Pluto
surface
Pluto
Atmosphere
Evidence that Pluto's atmosphere does not collapse from occultations including the 2013 May 04 event
artículo
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URL
https://digital.csic.es/bitstream/10261/167246/1/IAA_2015_Icarus_olkin.pdf
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169fe9e2771971b01397ae8690b2624b
997069
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IAA_2015_Icarus_olkin.pdf