Modelling oxygen isotopes in the UVic Earth System Climate Model under preindustrial and Last Glacial Maximum conditions: impact of glacial-interglacial sea ice variability on seawater d18O
Implementing oxygen isotopes (H218O, H216O) in coupled climate models provides both an important test of the individual model's hydrological cycle, and a powerful tool to mechanistically explore past climate changes while producing results directly comparable to isotope proxy records. The addi...
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| Language: | English en |
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2012
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| Online Access: | http://hdl.handle.net/1828/4261 |