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The development of the climate and Earth system models has had a long history, starting with the building of individual atmospheric, ocean, sea ice, land vegetation, biogeochemical, glacial and ecological model components. The early researchers were much aware of the long-term goal of building the Earth system models that would go beyond what is usually included in the climate models by adding interactive biogeochemical interactions. In the early days, the progress was limited by computerdoi:10.1098/rsta.2008.0219 pmid:19087933 fatcat:ps5gkl4cdrdplcgttmgvqn6sfq