Impact of vegetation feedback on the mid-Pliocene warm climate
Impact of vegetation feedback on the mid-Pliocene warm climate
复制标题
植被反馈对上新世中期温暖气候的影响
DOI：
10.1007/s00376-014-4015-5
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发表时间：
2014-09
影响因子：
5.8
通讯作者：
Jiang DB
中科院分区：
文献类型：
--
作者：
Zhang R;Zhang R;Jiang DB;Jiang DB
研究过去温暖时期的植被反馈可以更好地理解未来的植被反馈。在这项研究中，我们进行了几个模拟来分析中上新世暖期的植被反馈。结果表明，与工业化前相比，上新世中期植被变化的主要特征是针叶乔木北移，阔叶乔灌木扩展，草本植物北扩展。植被反馈引起的全球年平均增温率为12.1%，其中北部中高纬度地区的增温率较大。植被变化引起的增温与地表反照率变化直接相关，并被雪/海冰反照率反馈进一步放大。
Studying the vegetation feedback during warm periods of the past can lead to better understanding of those in the future. In this study, we conducted several simulations to analyze vegetation feedback during the mid-Pliocene warm period. The results indicate that the main features of vegetation change in the mid-Pliocene were a northward shift of needleleaf tree, an expansion of broadleaf tree and shrub, and a northward expansion of grass, as compared to the pre-industrial period. The global annual mean warming ratio caused by vegetation feedback was 12.1%, and this warming ratio was much larger in northern middle and high latitudes. The warming caused by vegetation change was directly related to the surface albedo change and was further amplified by snow/sea ice-albedo feedback.
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使用 NorESM-L 进行工业化前和上新世中期模拟：AGCM 模拟
DOI：
10.5194/gmd-5-1033-2012
发表时间：
2012-08
期刊：
Geosci. Model Dev.
影响因子：
--
作者：
Zhang Zhongshi;Yan Qing
通讯作者：
Yan Qing
影响因子：
4.8
作者：
W. Oleson;M. Lawrence;B. Bonan;G. Flanner;E. Kluzek;J. Lawrence;S. Levis;C. Swenson;E. Thor
通讯作者：
W. Oleson;M. Lawrence;B. Bonan;G. Flanner;E. Kluzek;J. Lawrence;S. Levis;C. Swenson;E. Thor
影响因子：
4.9
作者：
Gent, Peter R.;Danabasoglu, Gokhan;Zhang, Minghua
通讯作者：
Zhang, Minghua
DOI：
10.1002/joc.3527
发表时间：
2013-05
期刊：
International Journal of Climatology
影响因子：
--
作者：
Entao Yu;Huijun Wang;Jianqi Sun;Yongqi Gao
通讯作者：
Entao Yu;Huijun Wang;Jianqi Sun;Yongqi Gao
影响因子：
4.6
作者：
Ryouta O’ishi;A. Abe‐Ouchi
通讯作者：
Ryouta O’ishi;A. Abe‐Ouchi