arXiv subjects

M. B. Michaelis

Publications and source records attributed to M. B. Michaelis.

3 recordsLinked to original sources

arXiv2026

Spatial distribution of water ice in the protoplanetary silhouette disk d216-0939

The composition of rocky planets depends on the dust in their natal protoplanetary disk (PPD), potentially containing water ice. Crystalline water ice was detected in the PPD d216-0939 in the Orion Nebular Cluster (ONC). We aim at constraining the spatial distribution and crystallization state of water ice in the d216-0939 disk using recent observations of the water ice absorption feature at a wavelength of $\sim 3\mathrm{μm}$ collected with JWST. We perform 3D Monte Carlo radiative transfer (MCRT) simulations to constrain the free parameters of an accretion disk model by fitting the calculated spectrum in the wavelength range from $1.6 \text{ to } 24\mathrm{μm}$ to the spectral energy distribution (SED) observed with the JWST instruments NIRSpec and MIRI. Additionally, archival, spatially resolved HST observations were used to constrain the global spatial structure of the disk, as the parameter space is degenerate with respect to the fit to the SED. Successively, we fit the water ice absorption feature using polychromatic MCRT simulations with spectral importance sampling to produce synthetic observations at high spectral resolutions. By probing the upper and outer disk layers, we found that a PPD model with dust containing 5.4% crystallized water ice beyond the snowline fits the observations well, necessitating outward transport of material, since crystalline ice is unlikely to form in situ in the probed disk layers. In the spectral region of the water ice absorption feature, scattering and thermal dust emission both contribute significantly to the total flux.

astro-ph.EP↗

arXiv2026

Circular polarization as a probe of cloud properties and asymmetries in giant exoplanet atmospheres

For planets in the Solar System, circular polarization measurements complement linear polarimetry by providing additional information on cloud particle properties. As the disk-integrated circular polarization is 0 for symmetric planets, observing intrinsic circular polarization of spatially unresolved exoplanets requires stable spatial asymmetries such as circumplanetary rings. We investigated the potential of circular polarization measurements at optical and near-infrared wavelengths to determine optical properties of cloud particles in the atmospheres of giant exoplanets and characterize asymmetries. For 20 selected cloud condensates spanning a wide range of refractive indices, we calculated optical properties using Mie scattering theory. The circular polarization of starlight scattered by cloudy exoplanets was calculated with Monte Carlo radiative transfer simulations. To explain the connection between optical properties and planetary circular polarization, we derived an interpretative model of the first two scattering orders. Planetary hemispheres with atmospheres including cloud particles with a large imaginary part, $k$, of the refractive index show distinct circular polarization phase curves dominated by scattering first by gaseous molecules and then by cloud particles. The intrinsic degree of circular polarization, $P_\mathrm{c}$, is at most $3\cdot 10^{-4}$. When the cloud particles have a low $k$, they instead induce even smaller but more predictable circular polarization dominated by scattering solely by cloud particles. Circular polarization of starlight reflected by giant exoplanets is sensitive to cloud particle composition and large-scale asymmetries but remains a subtle signal. While promising for characterizing clouds under favorable conditions, practical detection requires technological advances in polarimetry and careful disentanglement from stellar background signals.

astro-ph.EP↗

arXiv2025

Polarimetry of exoplanet-exomoon systems

We investigated the potential of polarimetric observations in the optical wavelength range for the detection of exomoons and the characterization of exoplanet-exomoon systems. Using the three-dimensional Monte Carlo radiative transfer code POLARIS, we calculated flux and polarization phase curves of Earth-like exoplanets with a satellite similar to Earth's moon. Of particular interest are mutual events, when one of the two bodies casts a shadow on the other or transits in front of it. We find that the signatures of mutual events in the polarization phase curve show significant variations depending on the inclination of the lunar orbit. If the planet-satellite pair is spatially resolved from the star but the satellite is spatially unresolved, the increase in the degree of polarization during a transit of the exomoon in front of the center of the exoplanet reaches $2.7\%$ in our model system near quadrature. However, the change is less than $0.5\%$ if the orbit of the exomoon is inclined such that it transits the planet noncentrally at the same phase angles. The influence of an exomoon on the polarization phase curve of an exoplanet-exomoon system is dependent on the lunar polarization phase curve. Observations of full eclipses and occultations of the exomoon allow the determination of separate polarization phase curves for the two bodies. Information about the lunar orbital inclination can be obtained with polarimetric observations of shadows or transits. Measuring the influence of large satellites not only on the total flux, but also on the polarization of the reflected stellar radiation during mutual events thus facilitates the prediction of future mutual events and the verification of exomoon candidates.

astro-ph.EP↗