4.5 Article

The haze and methane distributions on Neptune from HST-STIS spectroscopy

期刊

ICARUS
卷 211, 期 1, 页码 780-797

出版社

ACADEMIC PRESS INC ELSEVIER SCIENCE
DOI: 10.1016/j.icarus.2010.08.013

关键词

Atmospheres, Composition; Atmospheres, Structure; Neptune; Neptune, Atmosphere; Spectroscopy

资金

  1. NASA [NNX08AE74G, NAS5-26555]
  2. NASA through a grant from the Space Telescope Science Institute [HST-GO-09330.01-A]

向作者/读者索取更多资源

We analyzed a data cube of Neptune acquired with the Hubble STIS spectrograph on August 3, 2003. The data covered the full afternoon hemisphere at 0.1 arcsec spatial resolution between 300 and 1000 nm wavelength at 1 nm resolution. Navigation was accurate to 0.004 arcsec and 0.05 nm. We constrained the vertical aerosol structure with radiative transfer calculations. Ultraviolet data confirmed the presence of a stratospheric haze of optical depth 0.04 at 370 nm wavelength. Bright, discrete clouds, most abundant near latitudes -40 degrees and 30 degrees, had their top near the tropopause. They covered 1.7% of the observed disk if they were optically thick. The methane abundance above the cloud tops was 0.0026 and 0.0017 km-am for southern and northern clouds, respectively, identical to earlier observations by Sromovsky et al. (Sromovsky, LA., Fry, P.M., Dowling, T.E., Baines, K.H., Limaye, S.S., [2001b]. Icarus 149, 459-488). Aside from these clouds, the upper troposphere was essentially clear. Below the 1.4-bar layer, a vertically uniform haze extended at least down to 10 bars with optical depth of 0.10-0.16/bar, depending on the latitude. Haze particles were bright at wavelengths above 600 nm, but darkened toward the ultraviolet, at the equator more so than at mid and high latitudes. A dark band near -60 degrees latitude was caused by a 0.01 decrease of the single scattering albedo in the visible, which was close to unity. A comparison of methane and hydrogen absorptions contradicted the current view that methane is uniformly mixed in latitude and altitude below the similar to 1.5-bar layer. The 0.04 +/- 0.01 methane mixing ratio is only uniform at low latitudes. At high southern latitudes, it is depressed roughly between the 1.2 and 3.3-bar layers compared to low-latitude values. The maximum depression factor is similar to 2.7 at 1.8 bars. We present models with 2 latitude sampling across the full sunlit globe that fit the observed reflectivities to 2.8% rms. (C) 2010 Elsevier Inc. All rights reserved.

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