Abstract:Previous modeling studies of Titan's dayside ionosphere predict electron number densities that are roughly a factor of 2 higher than those observed by the RPWS/Langmuir probe. The issue can equivalently be described as the ratio between the calculated electron production rates and the square of the observed electron number densities resulting in roughly a factor of 4 higher effective recombination coefficient than expected from the ion composition and the electron temperature.Here we make an extended reassessm… Show more
“…However, one should also consider a possible effect of the active ion chemistry happening in these regions on the characteristics of the electron population P3. In particular, the ionosphere environment on the nightside close to the terminator is enabling the growth of large ions, which is otherwise disrupted under direct extreme UV fluxes (Shebanits et al, 2017b(Shebanits et al, , 2017aWellbrock et al, 2019).…”
Section: Discussion On the Origin Of P3mentioning
confidence: 99%
“…Nevertheless, model results either predict too cold electrons (<0.02 eV; <200 K) at 900 km (Mukundan & Bhardwaj, 2018; Richard et al., 2011) or an overestimated electron density by a factor of two (Vigren et al., 2013, 2016). The addition of the negative ions to a photoionization model has been shown to decrease the discrepancy with the measurements (Shebanits, Vigren, Wahlund, Edberg, et al., 2017).…”
The Cassini Langmuir probe dataset in Titan's ionosphere is re-analyzed with a specific interest on the electron density and temperature. 2 to 4 cold electron populations with distinct potentials are observed. Electron populations vary with altitude and solar illumination suggesting origins linked to solar photons, magnetospheric particles and dust
“…However, one should also consider a possible effect of the active ion chemistry happening in these regions on the characteristics of the electron population P3. In particular, the ionosphere environment on the nightside close to the terminator is enabling the growth of large ions, which is otherwise disrupted under direct extreme UV fluxes (Shebanits et al, 2017b(Shebanits et al, , 2017aWellbrock et al, 2019).…”
Section: Discussion On the Origin Of P3mentioning
confidence: 99%
“…Nevertheless, model results either predict too cold electrons (<0.02 eV; <200 K) at 900 km (Mukundan & Bhardwaj, 2018; Richard et al., 2011) or an overestimated electron density by a factor of two (Vigren et al., 2013, 2016). The addition of the negative ions to a photoionization model has been shown to decrease the discrepancy with the measurements (Shebanits, Vigren, Wahlund, Edberg, et al., 2017).…”
The Cassini Langmuir probe dataset in Titan's ionosphere is re-analyzed with a specific interest on the electron density and temperature. 2 to 4 cold electron populations with distinct potentials are observed. Electron populations vary with altitude and solar illumination suggesting origins linked to solar photons, magnetospheric particles and dust
“…Nevertheless, model results either predict too cold electrons (< 0.02 eV; < 200 K) at 900 km (Mukundan & Bhardwaj, 2018;Richard et al, 2011) or an overestimated electron density by a factor of 2 (Vigren et al, 2013(Vigren et al, , 2016. The addition of the negative ions to a photoionisatoin model has been shown to decrease the discrepancy with the measurements (Shebanits et al, 2017a).…”
The Cassini Langmuir probe dataset in Titan's ionosphere is re-analyzed with a specific interest on the electron density and temperature. 2 to 4 cold electron populations with distinct potentials are observed. Electron populations vary with altitude and solar illumination suggesting origins linked to solar photons, magnetospheric particles and dust
“…Electron density and temperature were deduced from these measurements (Ågren et al., 2009; Edberg et al., 2010, 2013b, 2015; Wahlund et al., 2005). However, electron temperature measurements are not well reproduced by models of the ionosphere of Titan below 1,200 km: model results give electrons too cold by a factor of 2–3 (Galand et al., 2014; Mukundan & Bhardwaj, 2018; Richard et al., 2011; Shebanits, Vigren, Wahlund, Edberg, et al., 2017; Vigren et al., 2013, 2016).…”
The ionosphere of Titan hosts a complex ion chemistry leading to the formation of organic dust below 1,200 km. Current models cannot fully explain the observed electron temperature in this dusty environment. To achieve new insight, we have re‐analyzed the data taken in the ionosphere of Titan by the Cassini Langmuir probe (LP), part of the Radio and Plasma Wave Science package. A first paper (Chatain et al., 2021) introduces the new analysis method and discusses the identification of four electron populations produced by different ionization mechanisms. In this second paper, we present a statistical study of the whole LP dataset below 1,200 km which gives clues on the origin of the four populations. One small population is attributed to photo‐ or secondary electrons emitted from the surface of the probe boom. A second population is systematically observed, at a constant density (∼500 cm−3), and is attributed to background thermalized electrons from the ionization process of precipitating particles from the surrounding magnetosphere. The two last populations increase in density with pressure, solar illumination and Extreme ultraviolet flux. The third population is observed with varying densities at all altitudes and solar zenith angles (SZA) except on the far nightside (SZA > ∼140°), with a maximum density of 2,700 cm−3. It is therefore certainly related to the photo‐ionization of the atmospheric molecules. Finally, a fourth population detected only on the dayside and below 1,200 km reaching up to 2000 cm−3 could be photo‐ or thermo‐emitted from dust grains.
scite is a Brooklyn-based organization that helps researchers better discover and understand research articles through Smart Citations–citations that display the context of the citation and describe whether the article provides supporting or contrasting evidence. scite is used by students and researchers from around the world and is funded in part by the National Science Foundation and the National Institute on Drug Abuse of the National Institutes of Health.