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Перевод: radiative
[прилагательное] излучающий
Тезаурус:
- In the model the Arctic ozone hole appeared as a direct result of the changes in circulation induced by both doubling the amount of CO 2 and properly representing the radiative feedbacks of the evolving ozone distribution.
- Changes in stratospheric water vapour due to changes in methane and stratosphere-troposphere exchange could affect both the radiative budget and the temperature of PSC formation.
- When the concentration of CO 2 was doubled, the area of depleted ozone increased, but otherwise there was little change in the ozone behaviour, except when the effects of ozone radiative feedbacks were included in the model.
- Here we analyse the effects of increases in CO 2 and radiative feedbacks on the evolution of polar ozone in a three-dimensional model.
- P. R. Fontana's aims to give, in Atomic Radiative Processes , a unified treatment of classical and quantum theory, together with a description of atomic radiative processes.
- With current CO 2 and with radiative heating rates calculated using climatological ozone, high-latitude mean temperatures remained low until the occurrence of a stratospheric warming in late February (Fig. 1 a).
- Because there is no ozone radiative feedback in either simulation, the dynamical evolutions are identical, and therefore differences are due entirely to the changes in chemistry.
- Trace gases in the atmosphere are key components of the cycles of such elements as carbon, nitrogen, oxygen, sulphur and the halogens; as is now well known, their concentrations are much influenced by biogenic and anthropogenic activities and the concentrations of such gases as carbon dioxide, ozone, methane, nitrous oxide and the chlorofluoromethanes (CFMs) strongly affect radiative transfer and provide a link with the physical climate system.
- For consistency, the same ozone field was used in the radiative calculation but updated during the course of the simulations using either climatological or model-calculated values.
- Also, a detailed treatment of radiative heating and cooling takes account of the concentration of CO 2 and the distribution of ozone.
- Moreover, the reductions in ozone itself could produce some positive feedback by further reducing the radiative heating and hence the temperature of the lower stratosphere.
- Similar behaviour was also obtained with fully interactive ozone, but because of the radiative coupling of the ozone field to the dynamical evolution it was not possible to identify unambiguously the contributions of heterogeneous and homogeneous chemistry.
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