6 research outputs found
The First Post-Kepler Brightness Dips of KIC 8462852
We present a photometric detection of the first brightness dips of the unique variable star KIC 8462852 since the end of the Kepler space mission in 2013 May. Our regular photometric surveillance started in October 2015, and a sequence of dipping began in 2017 May continuing on through the end of 2017, when the star was no longer visible from Earth. We distinguish four main 1-2.5% dips, named "Elsie," "Celeste," "Skara Brae," and "Angkor", which persist on timescales from several days to weeks. Our main results so far are: (i) there are no apparent changes of the stellar spectrum or polarization during the dips; (ii) the multiband photometry of the dips shows differential reddening favoring non-grey extinction. Therefore, our data are inconsistent with dip models that invoke optically thick material, but rather they are in-line with predictions for an occulter consisting primarily of ordinary dust, where much of the material must be optically thin with a size scale <<1um, and may also be consistent with models invoking variations intrinsic to the stellar photosphere. Notably, our data do not place constraints on the color of the longer-term "secular" dimming, which may be caused by independent processes, or probe different regimes of a single process
Aerosol dynamics in ship tracks
Ship tracks are a natural laboratory to isolate the effect of anthropogenic
aerosol emissions on cloud properties. The Monterey Area Ship Tracks (MAST)
experiment in the Pacific Ocean west of Monterey, California, in June 1994, provides
an unprecedented data set for evaluating our understanding of the formation and
persistence of the anomalous cloud features that characterize ship tracks. The
data set includes conditions in which the marine boundary layer is both clean
and continentally influenced. Two case studies during the MAST experiment are
examined with a detailed aerosol microphysical model that considers an external
mixture of independent particle populations. The model allows tracking individual
particles through condensational and coagulational growth to identify the source
of cloud condensation nuclei (CCN). In addition, a cloud microphysics model was
employed to study specific effects of precipitation. Predictions and observations
reveal important differences between clean (particle concentrations below 150 cm -3)
and continentally influenced (particle concentrations above 400 cm-3 ) background
conditions: in the continentally influenced conditions there is a smaller change in
the cloud effective radius, drop number and liquid water content in the ship track
relative to the background than in the clean marine case. Predictions of changes
in cloud droplet number concentrations and effective radii are consistent with
observations although there is significant uncertainty in the absolute concentrations
due to a lack of measurements of the plume dilution. Gas-to-particle conversion of
sulfur species produced by the combustion of ship fuel is predicted to be important
in supplying soluble aerosol mass to combustion-generated particles, so as to render
them available as CCN. Studies of the impact of these changes on the cloud's
potential to precipitate concluded that more complex dynamical processes must be
represented to allow sufficiently long drop activations for drizzle droplets to form.This analysis was supported by NSF grant ATM-9732949 and ONR grant N00014-97-1- 0673. The aerosol measurements on which this work was based were supported by ONR grant N00014-93-1-0872
Retrieval of aerosol optical depth over land using two-angle view satellite radiometry during TARFOX
Comparison of risk of radiogenic second cancer following photon and proton craniospinal irradiation for a pediatric medulloblastoma patient
Pediatric patients who received radiation therapy are at risk of developing side effects like radiogenic second cancer. We compared proton and photon therapies in terms of the predicted risk of second cancers for a 4-year-old medulloblastoma patient receiving craniospinal irradiation (CSI). Two CSI treatment plans with 23.4 Gy or Gy (RBE) prescribed dose were computed: a three-field 6-MV photon therapy plan and a four-field proton therapy plan. The primary doses for both plans were determined using a commercial treatment planning system. Stray radiation doses for proton therapy were determined from Monte Carlo simulations, and stray radiation doses for photon therapy were determined from measured data. Dose-risk models based on the Biological Effects of Ionization Radiation VII report were used to estimate risk of second cancer in eight tissues/organs. Baseline predictions of the relative risk for each organ were always less for proton CSI than for photon CSI at all attained ages. The total lifetime attributable risks of the incidence of second cancer considered after proton CSI and photon CSI were 7.7% and 92%, respectively, and the ratio of lifetime risk was 0.083. Uncertainty analysis revealed that the qualitative findings of this study were insensitive to any plausible changes of dose-risk models and mean radiation weighting factor for neutrons. Proton therapy confers lower predicted risk of second cancer than photon therapy for the pediatric medulloblastoma patient