Prigent, C., J.R. Pardo, M.I. Mishchenko, and W.B. Rossow, 2001: Microwave polarized scattering signatures in clouds: Special Sensor Microwave / Imager (SSM / I) observations interpreted with
radiative transfer simulations.
We aim at analyzing observations of the polarized dust emission by disentangling the effects on the polarization signal in the context of 3D
radiative transfer simulations.
Not exact matches
A particular emphasis of Hayward's research is on combining hydrodynamic
simulations of galaxy formation with
radiative transfer calculations to create «forward models» of observable quantities, such as images and spectra, that can be directly compared with data from telescopes such as the Hubble Space Telescope.
In the following, after a description of the used
radiative transfer model we show spectrally resolved typical
simulations of atmospheric transmission and OLR for a standard atmospheric situation.
It's still qualitative however, and getting a better handle on the question requires
radiative transfer modeling and
simulations that can adequately handle a greenhouse - free atmosphere without blowing up.
We report the results of
simulations using a coupled ocean - atmosphere vector
radiative transfer code (NASA GISS) to obtain the polarized reflectance for various water compositions typical for coastal zones, as function of wavelength and sun / sensor geometry.
The
simulations have been performed using the
radiative transfer model MODTRAN.
My published works span many topics including convective heat
transfer,
radiative heat
transfer, fluid mechanics, and numerical
simulation.
The differences in radiatively active species and the formulation of
radiative transfer affect both the 19th - and 20th - century
simulations and the scenario integrations initiated from these historical
simulations.
Effects of bias in solar
radiative transfer codes on global climate model
simulations (Geophysical Research Letters, Vol.
«
Radiative transfer in model atmospheres including CO2, water vapor, ozone, and clouds can be explored by computer
simulation for the purpose of predicting the mean temperature at the surface of the earth.