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Contribution of oceanic and vegetation feedbacks to Holocene climate change in monsoonal Asia

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Figure

Table 1. Start day and length of the seasons for the mid-Holoceneand present-day orbital configuration, respectively.The seasonsare defined on astronomical calendar, based on the time of vernaland autumnal equinox as well as summer and winter solstice
Fig. 1. Location of the areas we consider in our feedback study.
Fig. 2. Seasonal and annual averaged 2m-temperature anomalies [K] between mid-Holocene and present-day climate resulting from thecoupled experiment AOV
Fig. 3. Same as Fig. 2, but for seasonal and annual averaged precipitation anomalies [mm/day]
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