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- W1785347804 abstract "Abstract The presently developed MPI/UW 3D — Earth system model for long-term integrations is applied to simulate the climate of the last interglacial. The model consists of an atmospheric and oceanic general circulation model, a dynamical terrestrial vegetation model and a marine carbon cycle model. The model was forced with time-varying insolation from 129000 to 113000 years before present (yr BP), revealing substantial feedbacks from the land biosphere on climate. These turned out to be important both for the simulated temperature in high northern latitudes and for the precipitation in the northern hemisphere monsoon belt. During the Eemian warm period, the simulated boreal forest extends in many places till the Arctic Ocean, and during the following cold period the transition between tundra and taiga migrated further south. Furthermore, associated albedo changes strongly amplify the simulated temperature changes. The intensified summer insolation during the Eemian leads to a higher precipitation over continents in the northern hemisphere. The strongest response is seen in the tropics and the African-Asian monsoon belt due to increased land-sea temperature contrasts. Vegetation is established in the Western Sahara desert. Compared to simulations with land vegetation prescribed at presentday pattern, the amount of precipitation in the Sahara is more than twice as large. The simulations show strong impacts on the time-transient climate response by triggering nonlinear delays and accelerations seen in various atmospheric and oceanic temperature time series. The simulated storage of carbon in the terrestrial biosphere is relatively large. The carbon storage in land vegetation is increased by more than 10% during the Eemian compared to the following cold period. The associated changes in storage in soil and litter account for more than 100 GtC." @default.
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- W1785347804 date "2007-01-01" @default.
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- W1785347804 title "37. Vegetation-climate feedbacks in transient simulations over the last interglacial (128 000-113 000 yr BP)" @default.
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- W1785347804 doi "https://doi.org/10.1016/s1571-0866(07)80062-5" @default.
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