GSTDTAP  > 气候变化
DOI10.1029/2018GL079150
Ring Shadowing Effects on Saturn's Ionosphere: Implications for Ring Opacity and Plasma Transport
Hadid, L. Z.1; Morooka, M. W.1; Wahlund, J. -E.1; Moore, L.2; Cravens, T. E.3; Hedman, M. M.4; Edberg, N. J. T.1; Vigren, E.1; Waite, J. H., Jr.5; Perryman, R.5; Kurth, W. S.6; Farrell, W. M.7; Eriksson, A. I.1
2018-10-16
发表期刊GEOPHYSICAL RESEARCH LETTERS
ISSN0094-8276
EISSN1944-8007
出版年2018
卷号45期号:19页码:10084-10092
文章类型Article
语种英语
国家Sweden; USA
英文摘要

We present new results obtained by the Radio and Plasma Wave Science Langmuir probe on board Cassini during the Grand Finale. The total direct current sampled by the Langmuir probe at negative bias voltage is used to study the effect of the ring shadows on the structure of the Kronian topside ionosphere. The D and C rings and the Cassini Division are confirmed to be optically thin to extreme ultraviolet solar radiation. However, different responses from the opaque A and B rings are observed. The edges of the A ring shadow are shown to match the A ring boundaries, unlike the B ring, which indicates variable responses to the B ring shadow. We show that the variable responses are due to the ionospheric plasma, more precisely to the longer chemical lifetime of H+ compared to H-2(+) and H-3(+), suggesting that the plasma is transported from the sunlit region to the shadowed one in the ionosphere.


Plain Language Summary As Saturn's northern hemisphere experienced summer during the Grand Finale, the planet's northern dayside hemisphere and its rings were fully illuminated by the Sun. However, the southern hemisphere was partly obscured because of the shadows cast by the A and B rings. Using the in situ measurements of the Langmuir probe part of the Radio and Plasma Wave Science investigation on board the Cassini spacecraft, we study for the first time the effect of the ring shadows on Saturn's ionosphere. From the ring shadows signatures on the total ion current collected by the Langmuir probe, we show that the A and B rings are optically thicker (to the solar extreme ultraviolet radiation) than the inner C and D rings and the Cassini Division to the solar extreme ultraviolet radiation. Moreover, we reproduce the boundaries of the A ring and the outer edge of the B ring. Furthermore, observed variations with respect to the inner edge of the B ring imply a delayed response of the ionospheric H+ because of its long lifetime and suggest that the ionospheric plasma is transported from an unshadowed region to a shadowed one in the ionosphere.


领域气候变化
收录类别SCI-E
WOS记录号WOS:000448656800007
WOS关键词ION DENSITIES ; RADIO ; SYSTEM
WOS类目Geosciences, Multidisciplinary
WOS研究方向Geology
引用统计
文献类型期刊论文
条目标识符http://119.78.100.173/C666/handle/2XK7JSWQ/27937
专题气候变化
作者单位1.Swedish Inst Space Phys, Uppsala, Sweden;
2.Boston Univ, Ctr Space Phys, Boston, MA 02215 USA;
3.Univ Kansas, Dept Phys & Astron, Lawrence, KS 66045 USA;
4.Univ Idaho, Dept Phys, Moscow, ID USA;
5.Southwest Res Inst, Space Sci & Engn Div, San Antonio, TX USA;
6.Univ Iowa, Dept Phys & Astron, Iowa City, IA 52242 USA;
7.NASA, Goddard Space Flight Ctr, Greenbelt, MD USA
推荐引用方式
GB/T 7714
Hadid, L. Z.,Morooka, M. W.,Wahlund, J. -E.,et al. Ring Shadowing Effects on Saturn's Ionosphere: Implications for Ring Opacity and Plasma Transport[J]. GEOPHYSICAL RESEARCH LETTERS,2018,45(19):10084-10092.
APA Hadid, L. Z..,Morooka, M. W..,Wahlund, J. -E..,Moore, L..,Cravens, T. E..,...&Eriksson, A. I..(2018).Ring Shadowing Effects on Saturn's Ionosphere: Implications for Ring Opacity and Plasma Transport.GEOPHYSICAL RESEARCH LETTERS,45(19),10084-10092.
MLA Hadid, L. Z.,et al."Ring Shadowing Effects on Saturn's Ionosphere: Implications for Ring Opacity and Plasma Transport".GEOPHYSICAL RESEARCH LETTERS 45.19(2018):10084-10092.
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