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Radiation Effects on Carrier Transport
1999The model equations and boundary conditions reviewed in the preceding chapter describe electrical transport in semiconductor microtransducers in the absence of external fields. As summarized in Sect. 2.7, external fields appreciably alter carrier transport by introducing asymmetries in device operation.
Arokia Nathan, Henry Baltes
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Radiation transport with anisotropic scattering
Journal of Quantitative Spectroscopy and Radiative Transfer, 1974Abstract Reflection and transmission of radiation with anisotropic scattering in considered, using an invariant-imbedding formulation of the transport equation. Extensive numerical calculations show that the results of the transport approximation, in which the scattering kernel is represented by an isotropic part and a forward scattered component ...
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Partial redistribution in radiation transport
Journal of Quantitative Spectroscopy and Radiative Transfer, 1972Abstract Radiation diffusion in a slab of purely scattering atoms with only one transition is calculated using a Monte Carlo method. Partial redistribution because of the Doppler effect is included. The scattering is assumed to be isotropic and incoherent. Results are obtained for (1) the amount of diffuse reflection and transmission as a function of
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Non-Equilibrium Radiation Transport
1969To calculate the radiative properties of a gas it is necessary that the occupation numbers of the various atomic states of the gas particles be known. If the gas is in LTE, the occupation numbers can be expressed in terms of the local temperature and atomic parameters by using standard statistical mechanics.
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Science of Climate Change
We briefly review the dominant role of clouds in Earth’s climate. The earliest observational studies of heat transfer through Earth’s atmosphere, for example, those of John Leslie around 1800, showed that clouds have a large effect on radiative heat transfer from Earth’s surface to space.
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We briefly review the dominant role of clouds in Earth’s climate. The earliest observational studies of heat transfer through Earth’s atmosphere, for example, those of John Leslie around 1800, showed that clouds have a large effect on radiative heat transfer from Earth’s surface to space.
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