Search engine for discovering works of Art, research articles, and books related to Art and Culture
ShareThis
Javascript must be enabled to continue!

The spatial distribution of dust in the inner comae of comets: Evidence for and modelling of nightside emission

View through CrossRef
<p>Spacecraft imaging of the inner comae of 1P/Halley (Giotto/HMC) and 19P/Borrelly (DS1/MICAS) indicated unexpectedly low ratios for the dust brightness above the dayside hemisphere to that above the nightside. Neither ratio was consistent with dust emission being directly proportional to sublimation loss of H2O using purely insolation-driven models. The near-terminator observations of 67P/Churyumov-Gerasimenko from Rosetta allow very precise separation of the dayside and nightside hemispheres and confirm low dayside to nightside dust brightness ratios. In the case of 67P values of ~3.3:1 were observed and an interesting trend towards increased ratios with decreasing heliocentric distance. Detailed modelling using insolation-driven models do not fit the data by factors of several. Dust from the dayside may contribute to the brightness on the nightside if particles are not escaping and therefore gravitationally bound. However, the radial distribution of brightness on the nightside is inconsistent with this interpretation as can be demonstrated with a simple model. The source is also not in the form of single nightside (e.g. “sunset”) jets. Furthermore, shadowing of emitted dust by the nucleus itself indicates that much of the observed brightness on the nightside is very close to the nucleus and distributed roughly uniformly around in the nightside hemisphere (Gerig et al., submitted).</p><p>Gas emission from the nightside has been a consistent element of source distributions (e.g. Bieler et al., 2015) required to model ROSINA/COPS data. However, the composition is frequently not specified. We have been investigating self-consistent, physically generated, numerical models of combined H2O and CO2 emission (see also Herny et al., submitted). Dust emission has been incorporated into the model chain allowing modelling of the observation of the gas composition, the gas density, and the dust brightness distribution in the vicinity of the nucleus for specific times. The results of investigation will be presented.</p>
Title: The spatial distribution of dust in the inner comae of comets: Evidence for and modelling of nightside emission
Description:
<p>Spacecraft imaging of the inner comae of 1P/Halley (Giotto/HMC) and 19P/Borrelly (DS1/MICAS) indicated unexpectedly low ratios for the dust brightness above the dayside hemisphere to that above the nightside.
Neither ratio was consistent with dust emission being directly proportional to sublimation loss of H2O using purely insolation-driven models.
The near-terminator observations of 67P/Churyumov-Gerasimenko from Rosetta allow very precise separation of the dayside and nightside hemispheres and confirm low dayside to nightside dust brightness ratios.
In the case of 67P values of ~3.
3:1 were observed and an interesting trend towards increased ratios with decreasing heliocentric distance.
Detailed modelling using insolation-driven models do not fit the data by factors of several.
Dust from the dayside may contribute to the brightness on the nightside if particles are not escaping and therefore gravitationally bound.
However, the radial distribution of brightness on the nightside is inconsistent with this interpretation as can be demonstrated with a simple model.
The source is also not in the form of single nightside (e.
g.
“sunset”) jets.
Furthermore, shadowing of emitted dust by the nucleus itself indicates that much of the observed brightness on the nightside is very close to the nucleus and distributed roughly uniformly around in the nightside hemisphere (Gerig et al.
, submitted).
</p><p>Gas emission from the nightside has been a consistent element of source distributions (e.
g.
Bieler et al.
, 2015) required to model ROSINA/COPS data.
However, the composition is frequently not specified.
We have been investigating self-consistent, physically generated, numerical models of combined H2O and CO2 emission (see also Herny et al.
, submitted).
Dust emission has been incorporated into the model chain allowing modelling of the observation of the gas composition, the gas density, and the dust brightness distribution in the vicinity of the nucleus for specific times.
The results of investigation will be presented.
</p>.

Related Results

Linear polarization as a tool to characterize interplanetary, cometary, and extrasolar dust particles
Linear polarization as a tool to characterize interplanetary, cometary, and extrasolar dust particles
SummaryLinear polarization observations have suggested the presence of dust particles that scatter solar light within cometary comae and the interplanetary dust cloud. Recent progr...
Physical Evolution Model for Jupiter-Family Comets and Centaurs
Physical Evolution Model for Jupiter-Family Comets and Centaurs
Centaurs – planet-crossing bodies in the region of the giant planets that mainly originate in the Kuiper Belt/Scattered Disk [1, 2] – are thought to be the prim...
FeI and NiI in comets
FeI and NiI in comets
Metals have been found in cometary dust by in-situ experiments onboard the Giotto and Rosetta spacecrafts[4,10] as well as in dust particles collected by the Stardust spacecraft[11...
Distribution of long-period comets: comparison between simulations and observations
Distribution of long-period comets: comparison between simulations and observations
Aims. This paper is devoted to a comparison between observations and simulations of the so-called Oort spike formed by the “new” observable long-period comets. Methods. The...
The effect of thermal inertia on the outgassing and gas dynamics in the inner-coma of cometary nuclei
The effect of thermal inertia on the outgassing and gas dynamics in the inner-coma of cometary nuclei
There is a basic understanding of the way gases are released from cometary nuclei in order to form the gas and dust comae as they approach the Sun. We know that the production of t...
Dust deposition and lifting at the Zhurong landing site
Dust deposition and lifting at the Zhurong landing site
IntroductionDust deposition poses the challenges to the survival of instruments and solar-powered missions on Mars [1, 2]. Zhurong in-situ observations provide an opportunity to st...
Modelling trajectories of wind-blown particles in the Martian atmosphere
Modelling trajectories of wind-blown particles in the Martian atmosphere
AbstractMartian dust storms can obscure the lower reaches of the atmosphere from orbiting spacecraft and at the same time obscure the upper atmosphere from landed spacecraft. Infer...
Primitiveness of cometary dust collected by MIDAS on-board Rosetta
Primitiveness of cometary dust collected by MIDAS on-board Rosetta
<p>Comets are thought to have preserved dust particles from the beginning of Solar System formation, providing a unique insight into dust growth mechanisms. The Roset...

Back to Top