Article 6.3.4.3 Mathematical Models of Human-Induced Global Change

نویسنده

  • Alex Hall
چکیده

Complex mathematical models requiring major computing power to tease out their implications are currently the main theoretical tool used to understand and predict the response of the climate system to external forcing, such as that resulting from the current human perturbation to greenhouse gas concentrations in the atmosphere. These models developed quickly over the last half of the 20 century and are in use at several modeling centers around the world. They typically contain sub-models of the atmosphere, land, and ocean, and sometimes also the biosphere. They are used to simulate climate change by imposing an external forcing similar to what the real climate has experienced over the last century and is projected to experience in the coming one. Confidence in their predictions of the gross geographical distribution of temperature change is probably warranted. However, confidence in the overall magnitude of the simulated change is not, mainly due to the current inability to incorporate important climate feedbacks stemming from processes that cannot be explicitly resolved by the models, such as changes in cloudiness as climate warms. The models predict not only a temperature response to increasing greenhouse gas concentrations, but also an increase in the intensity of the global hydrologic cycle. Though there is reason to have some confidence in this globalscale prediction, the simulated regional-scale changes in the hydrologic cycle are almost certainly not trustworthy. Increasing confidence in model predictions in these critical areas will involve improving the dialogue between model and observations, as well as wise investment of additional computational resources.

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تاریخ انتشار 2004