Climate models are used for a variety of purposes from the study of dynamics of the weather and climate system to projections of future climate.
NOAA's Geophysical Fluid Dynamics Laboratory has created several ocean-atmosphere coupled models to predict how greenhouse gas emissions following different population, economic, and energy-use projections may affect the planet.
"Representative Concentration Pathways (RCPs) are not new, fully integrated scenarios (i.e., they are not a complete package of socioeconomic, emissions and climate projections). They are consistent sets of projections of only the components of radiative forcing that are meant to serve as input for climate modeling, pattern scaling and atmospheric chemistry modeling," according to the RCP Database.
Global climate models represent the planet as millions of grid boxes and then solve mathematical equations to calculate how energy is transferred between those boxes using the laws of thermodynamics. If done correctly, these models of how energy is cycled through all parts of the planet can be used to estimate dozens of environmental variables (winds, temperature, moisture, etc.). The models are tested by simulating historical conditions and then matching the results to our historical observational records. If the models can adequately recreate the past, they are then run forward in time to predict what may happen in the future.
Shown here are the predicted surface temperatures under the RCP 2.6 emissions scenario using GFDL's CM3 model. The CM3 is just one of many climate models that are analyzed to make predictions about our changing climate. The RCP 2.6 scenario is a so-called "peak" scenario, which means the radiative forcing level reaches 3.1 W/m2 by mid-century but returns to 2.6 W/m2 by 2100.
In this imagery, if temperature is colored red, it is predicted to be higher than the 20th century average; if it is blue, then it is predicted to be lower than average.
The Earth gets warmer as CO2 increases in the atmosphere
The Earth doesn't warm uniformly, the oceans warm slower than the continents and arctic
Projections are based on a high emissions scenario
Projections for temperature according to RCP 2.6 W/m2 show the level of radiative forcing by greenhouse gas emissions peaking by mid-century then returning to 2.6 W/m2 by 2100
A large-scale, global and differentiated greenhouse gas mitigation strategy and new technologies would need to be widely employed very soon in order to attain this reality of the scenario depicted here