Concurrent Calculation of Radiative Transfer in the Atmospheric Simulation in ECHAM-6.3.05p2 [PDF]
Abstract. The scalability of the atmospheric model ECHAM6 at low resolution, as used in palaeoclimate simulations, suffers from the limited number of grid points. As a consequence, the potential of current high performance computing architectures cannot be used at full scale for such experiments, particularly within the available domain-decomposition ...
M. R. Heidari +5 more
openaire +3 more sources
ARTS, the atmospheric radiative transfer simulator, version 2 [PDF]
The second version of the atmospheric radiative transfer simulator, ARTS, is introduced. This is a general software package for long wavelength radiative transfer simulations, with a focus on passive microwave observations.
Davis, C. P. +23 more
core +1 more source
Radiative forcing since preindustrial times due to ozone change in the troposphere and the lower stratosphere [PDF]
Changes in atmospheric ozone have occurred since the preindustrial era as a result of increasing anthropogenic emissions. Within ACCENT, a European Network of Excellence, ozone changes between 1850 and 2000 are assessed for the troposphere and the lower ...
Zeng, G +96 more
core +1 more source
A MODEL TO SIMULATE THE RADIATIVE TRANSFER OF FLUORESCENCE IN A LEAF [PDF]
Abstract. Light is reflected, transmitted and absorbed by green leaves. Chlorophyll fluorescence (ChlF) is the signal emitted by chlorophyll molecules in the leaf after the absorption of light. ChlF can be used as a direct probe of the functional status of photosynthetic machinery because of its close relationship with photosynthesis.
F. Zhao, Q. Ni
openaire +3 more sources
Calculation of the radiance distribution at the boundary of an isotropically scattering slab [PDF]
The radiance arising from an anisotropically scattering illuminated stack of n slabs is calculated using the equation of radiative transfer. It appears to be unnecessary to calculate the radiance inside the material; including only the radiance at the ...
Rinzema, K., +5 more
core +1 more source
Simulation of SEVIRI infrared channels: a case study from the Eyjafjallajökull April/May 2010 eruption [PDF]
Infrared satellite images are widely and successfully used to detect and follow atmospheric ash from erupting volcanoes. We describe a new radiative transfer model framework for the simulation of infrared radiances, which can be compared directly with ...
A. Kylling +5 more
doaj +1 more source
Is a scaling factor required to obtain closure between measured and modelled atmospheric O4 absorptions? An assessment of uncertainties of measurements and radiative transfer simulations for 2 selected days during the MAD-CAT campaign [PDF]
In this study the consistency between MAX-DOAS measurements and radiative transfer simulations of the atmospheric O4 absorption is investigated on 2 mainly cloud-free days during the MAD-CAT campaign in Mainz, Germany, in summer 2013.
T. Wagner +33 more
doaj +1 more source
Simulations of proton transfer processes using reactive force fields [PDF]
Within this thesis we presented the development of reactive force fields that are ca- pable to describe the dynamics of proton and hydrogen atom transfer processes.
Lammers, Sven
core +1 more source
ARTS, the atmospheric radiative transfer simulator
Abstract ARTS is a modular program that simulates atmospheric radiative transfer. The paper describes ARTS version 1.0, which is applicable in the absence of scattering. An overview over all major parts of the model is given: calculation of absorption coefficients, the radiative transfer itself, and the calculation of Jacobians.
Buehler, Stefan A. +4 more
openaire +3 more sources
Radiative forcing in the 21st century due to ozone changes in the troposphere and the lower stratosphere [PDF]
Radiative forcing due to changes in ozone is expected for the 21st century. An assessment on changes in the tropospheric oxidative state through a model intercomparison ("OxComp'') was conducted for the IPCC Third Assessment Report (IPCC-TAR).
Isaksen, I S A +92 more
core +1 more source

