globalchange  > 气候变化与战略
DOI: 10.5194/cp-8-565-2012
Scopus记录号: 2-s2.0-84863343614
论文题名:
Vegetation-climate interactions in the warm mid-Cretaceous
作者: Zhou J.; Poulsen C.J.; Rosenbloom N.; Shields C.; Briegleb B.
刊名: Climate of the Past
ISSN: 18149324
出版年: 2012
卷: 8, 期:2
起始页码: 565
结束页码: 576
语种: 英语
Scopus关键词: albedo ; atmosphere-biosphere interaction ; bare soil ; carbon dioxide ; Cretaceous ; forest ; fossil ; general circulation model ; heat transfer ; meridional circulation ; overturn ; paleoclimate ; paleoecology ; polar region ; precipitation (climatology) ; vegetation dynamics ; warming
英文摘要: 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 1x, 10x and 16x pre-industrial atmospheric CO 2. Results show that forests expand from mid-latitudes to high latitudes as CO 2 increases from 1x to 10x and 16x, mainly due to the CO 2-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 0.11 mm 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 CO 2 and high-latitude vegetation are required to maintain the polar warmth. © Author(s) 2012.
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/49616
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Recommended Citation:
Zhou J.,Poulsen C.J.,Rosenbloom N.,et al. Vegetation-climate interactions in the warm mid-Cretaceous[J]. Climate of the Past,2012-01-01,8(2)
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