Changes in the potential distribution of humid tropical forests on a warmer planet

被引:141
作者
Zelazowski, Przemyslaw [1 ]
Malhi, Yadvinder [1 ]
Huntingford, Chris [2 ]
Sitch, Stephen [3 ]
Fisher, Joshua B. [4 ]
机构
[1] Univ Oxford, Environm Change Inst, Sch Geog & Environm, Oxford OX1 3QY, England
[2] Ctr Ecol & Hydrol, Wallingford OX10 8BB, Oxon, England
[3] Univ Leeds, Sch Geog, Leeds LS2 9JT, W Yorkshire, England
[4] CALTECH, NASA, Jet Prop Lab, Pasadena, CA 91109 USA
来源
PHILOSOPHICAL TRANSACTIONS OF THE ROYAL SOCIETY A-MATHEMATICAL PHYSICAL AND ENGINEERING SCIENCES | 2011年 / 369卷 / 1934期
基金
英国自然环境研究理事会;
关键词
tropical forests; climate change; climate patterns; water stress; maximum climatological water deficit; carbon dioxide; GLOBAL VEGETATION MODELS; CLIMATE-CHANGE SCENARIOS; CARBON-CYCLE FEEDBACKS; ATMOSPHERE WATER FLUX; CHANGE IMPACTS; ANALOG MODEL; RAIN-FOREST; TEMPERATURE; DIEBACK; EVAPOTRANSPIRATION;
D O I
10.1098/rsta.2010.0238
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
The future of tropical forests has become one of the iconic issues in climate-change science. A number of studies that have explored this subject have tended to focus on the output from one or a few climate models, which work at low spatial resolution, whereas society and conservation-relevant assessment of potential impacts requires a finer scale. This study focuses on the role of climate on the current and future distribution of humid tropical forests (HTFs). We first characterize their contemporary climatological niche using annual rainfall and maximum climatological water stress, which also adequately describe the current distribution of other biomes within the tropics. As a first-order approximation of the potential extent of HTFs in future climate regimes defined by global warming of 2 degrees C and 4 degrees C, we investigate changes in the niche through a combination of climate-change anomaly patterns and higher resolution (5 km) maps of current climatology. The climate anomalies are derived using data from 17 coupled Atmosphere-Ocean General Circulation Models (AOGCMs) used in the Fourth Assessment of the Intergovernmental Panel for Climate Change. Our results confirm some risk of forest retreat, especially in eastern Amazonia, Central America and parts of Africa, but also indicate a potential for expansion in other regions, for example around the Congo Basin. The finer spatial scale enabled the depiction of potential resilient and vulnerable zones with practically useful detail. We further refine these estimates by considering the impact of new environmental regimes on plant water demand using the UK Met Office land- surface scheme (of the HadCM3 AOGCM). The CO2-related reduction in plant water demand lowers the risk of die-back and can lead to possible niche expansion in many regions. The analysis presented here focuses primarily on hydrological determinants of HTF extent. We conclude by discussing the role of other factors, notably the physiological effects of higher temperature.
引用
收藏
页码:137 / 160
页数:24
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