Determining solar effects in Neptune’s atmosphere

Long-duration observations of Neptune’s brightness at two visible wavelengths provide a disk-averaged estimate of its atmospheric aerosol. Brightness variations were previously associated with the 11-year solar cycle, through solar-modulated mechanisms linked with either ultraviolet or galactic cosm...

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Những tác giả chính: Aplin, K, Harrison, R
Định dạng: Journal article
Được phát hành: Nature Publishing Group 2016
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author Aplin, K
Harrison, R
author_facet Aplin, K
Harrison, R
author_sort Aplin, K
collection OXFORD
description Long-duration observations of Neptune’s brightness at two visible wavelengths provide a disk-averaged estimate of its atmospheric aerosol. Brightness variations were previously associated with the 11-year solar cycle, through solar-modulated mechanisms linked with either ultraviolet or galactic cosmic ray (GCR) effects on atmospheric particles. Here, we use a recently extended brightness data set (1972–2014), with physically realistic modelling to show, rather than alternatives, ultraviolet and GCR are likely to be modulating Neptune’s atmosphere in combination. The importance of GCR is further supported by the response of Neptune’s atmosphere to an intermittent 1.5- to 1.9-year periodicity, which occurred preferentially in GCR (not ultraviolet) during the mid-1980s. This periodicity was detected both at Earth, and in GCR measured by Voyager 2, then near Neptune. A similar coincident variability in Neptune’s brightness suggests nucleation onto GCR ions. Both GCR and ultraviolet mechanisms may occur more rapidly than the subsequent atmospheric particle transport.
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spelling oxford-uuid:8836e65e-af08-4ce6-81d5-be0e513861752022-03-26T22:15:40ZDetermining solar effects in Neptune’s atmosphereJournal articlehttp://purl.org/coar/resource_type/c_dcae04bcuuid:8836e65e-af08-4ce6-81d5-be0e51386175Symplectic Elements at OxfordNature Publishing Group2016Aplin, KHarrison, RLong-duration observations of Neptune’s brightness at two visible wavelengths provide a disk-averaged estimate of its atmospheric aerosol. Brightness variations were previously associated with the 11-year solar cycle, through solar-modulated mechanisms linked with either ultraviolet or galactic cosmic ray (GCR) effects on atmospheric particles. Here, we use a recently extended brightness data set (1972–2014), with physically realistic modelling to show, rather than alternatives, ultraviolet and GCR are likely to be modulating Neptune’s atmosphere in combination. The importance of GCR is further supported by the response of Neptune’s atmosphere to an intermittent 1.5- to 1.9-year periodicity, which occurred preferentially in GCR (not ultraviolet) during the mid-1980s. This periodicity was detected both at Earth, and in GCR measured by Voyager 2, then near Neptune. A similar coincident variability in Neptune’s brightness suggests nucleation onto GCR ions. Both GCR and ultraviolet mechanisms may occur more rapidly than the subsequent atmospheric particle transport.
spellingShingle Aplin, K
Harrison, R
Determining solar effects in Neptune’s atmosphere
title Determining solar effects in Neptune’s atmosphere
title_full Determining solar effects in Neptune’s atmosphere
title_fullStr Determining solar effects in Neptune’s atmosphere
title_full_unstemmed Determining solar effects in Neptune’s atmosphere
title_short Determining solar effects in Neptune’s atmosphere
title_sort determining solar effects in neptune s atmosphere
work_keys_str_mv AT aplink determiningsolareffectsinneptunesatmosphere
AT harrisonr determiningsolareffectsinneptunesatmosphere