Matches in DBpedia 2015-10 for { ?s ?p "This article is about the theories and mathematics of climate modeling. For computer-driven prediction of Earth's climate, see Global climate model.Climate models use quantitative methods to simulate the interactions of the important drivers of climate, including atmosphere, oceans, land surface and ice. They are used for a variety of purposes from study of the dynamics of the climate system to projections of future climate. The most talked-about use of climate models in recent years has been to project temperature changes resulting from increases in atmospheric greenhouse gas concentrations.All climate models take account of incoming energy from the sun as short wave electromagnetic radiation, chiefly visible and short-wave (near) infrared, as well as outgoing long wave (far) infrared electromagnetic. Any imbalance results in a change in temperature.Models vary in complexity: A simple radiant heat transfer model treats the earth as a single point and averages outgoing energy This can be expanded vertically (radiative-convective models) and/or horizontally Finally, (coupled) atmosphere–ocean–sea ice global climate models solve the full equations for mass and energy transfer and radiant exchange. Box models can treat flows across and within ocean basins. Other types of modelling can be interlinked, such as land use, allowing researchers to predict the interaction between climate and ecosystems."@en }
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- Climate_model abstract "This article is about the theories and mathematics of climate modeling. For computer-driven prediction of Earth's climate, see Global climate model.Climate models use quantitative methods to simulate the interactions of the important drivers of climate, including atmosphere, oceans, land surface and ice. They are used for a variety of purposes from study of the dynamics of the climate system to projections of future climate. The most talked-about use of climate models in recent years has been to project temperature changes resulting from increases in atmospheric greenhouse gas concentrations.All climate models take account of incoming energy from the sun as short wave electromagnetic radiation, chiefly visible and short-wave (near) infrared, as well as outgoing long wave (far) infrared electromagnetic. Any imbalance results in a change in temperature.Models vary in complexity: A simple radiant heat transfer model treats the earth as a single point and averages outgoing energy This can be expanded vertically (radiative-convective models) and/or horizontally Finally, (coupled) atmosphere–ocean–sea ice global climate models solve the full equations for mass and energy transfer and radiant exchange. Box models can treat flows across and within ocean basins. Other types of modelling can be interlinked, such as land use, allowing researchers to predict the interaction between climate and ecosystems.".