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- W4253744152 abstract "Abstract. Vegetation-climate interactions are thought to have amplified polar warmth during past warm periods. Here, we explore the vegetation-climate interactions in the mid- Cretaceous using a fully coupled ocean-atmosphere general circulation model with a dynamic vegetation component. We run simulations with 1×, 10× and 16× preindustrial atmospheric CO2. Results show that forests expand from mid-latitudes to high latitudes as CO2 increases from 1× to 10× and 16×, mainly due to the CO2- induced warming. This expansion of mid-to-high latitude forests are largely supported by the distribution of mid-Cretaceous fossil woods and coal deposits. Globally, the presence of vegetation increases mean annual temperature and precipitation by 0.9 °C and 0.11mm day−1 relative to bare ground. High-latitude warming induced by the presence of vegetation (∼1.9 °C) is less than half of that reported in previous studies. The weaker warming here is mainly due to less pronounced albedo feedbacks, and to a less extent, reduced poleward heat transport via weakening of the meridional overturning circulation. Our results suggest that other mechanisms in addition to high atmospheric CO2 and high-latitude vegetation are required to maintain the polar warmth." @default.
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- W4253744152 date "2011-09-07" @default.
- W4253744152 modified "2023-10-16" @default.
- W4253744152 title "Vegetation-climate interactions in the warm mid-Cretaceous" @default.
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- W4253744152 doi "https://doi.org/10.5194/cpd-7-2803-2011" @default.
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