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Spatial resolution specifies how large (in degrees of latitude and longitude or in km or miles) the grid cells in a model are. Temporal resolution refers to the size of the time steps used in models. How often (in simulated or “model time”) calculations of the various properties being modeled are conducted.
Climate Model Resolution The results of processes modeled in each cell are passed to neighboring cells to model the exchange of matter and energy over time. Grid cell size defines the resolution of the model: the smaller the size of the grid cells, the higher the level of detail in the model.
Climate models are important tools for improving our understanding and predictability of climate behavior on seasonal, annual, decade, and centennial time scales. Models investigate the degree to which observed climate changes may be due to natural variability, human activity, or a combination of both.
Scientists use climate models to understand complex earth systems. These models allow them to test hypotheses and draw conclusions on past and future climate systems. This can help them determine whether abnormal weather events or storms are a result of changes in climate or just part of the routine climate variation.
Climate Model Resolution The results of processes modeled in each cell are passed to neighboring cells to model the exchange of matter and energy over time. Grid cell size defines the resolution of the model: the smaller the size of the grid cells, the higher the level of detail in the model.
To predict future climate, scientists use computer programs called climate models to understand how our planet is changing. Climate models work like a laboratory in a computer. They allow scientists to study how different factors interact to influence a region's climate.
Building a 3-D map of the Earth's climate system. The basic building blocks of climate models are 3-D “grid cells” that contain climate-related physical information about a particular location. Developing computer code. Making the model run through time.
Climate models are constructed with two types of essential building blocks: physical, chemical, and biological laws founded on theory (the laws of thermodynamics and Newton's laws of motion, for example, are critical to understanding circulation) and data collected from observation.
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