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DOI10.1038/nature12434
Asymmetric effects of daytime and night-time warming on Northern Hemisphere vegetation
Peng, Shushi; Piao, Shilong; Ciais, Philippe; Myneni, Ranga B.; Chen, Anping; Chevallier, Frederic; Dolman, Albertus J.; Janssens, Ivan A.; Penuelas, Josep; Zhang, Gengxin; Vicca, Sara; Wan, Shiqiang; Wang, Shiping; Zeng, Hui
通讯作者Piao, S (通讯作者)
发表日期2013
ISSN0028-0836
EISSN1476-4687
起始页码88
结束页码+
卷号501期号:7465
英文摘要Temperature data over the past five decades show faster warming of the global land surface during the night than during the day(1). This asymmetric warming is expected to affect carbon assimilation and consumption in plants, because photosynthesis in most plants occurs during daytime and is more sensitive to the maximum daily temperature, T-max, whereas plant respiration occurs throughout the day(2) and is therefore influenced by both T-max and the minimum daily temperature, T-min. Most studies of the response of terrestrial ecosystems to climate warming, however, ignore this asymmetric forcing effect on vegetation growth and carbon dioxide (CO2) fluxes(3-6). Here we analyse the interannual covariations of the satellite-derived normalized difference vegetation index (NDVI, an indicator of vegetation greenness) with Tmax and Tmin over the Northern Hemisphere. After removing the correlation between Tmax and Tmin, we find that the partial correlation between Tmax and NDVI is positive in most wet and cool ecosystems over boreal regions, but negative in dry temperate regions. In contrast, the partial correlation between Tmin and NDVI is negative in boreal regions, and exhibits a more complex behaviour in dry temperate regions. We detect similar patterns in terrestrial net CO2 exchange maps obtained from a global atmospheric inversion model. Additional analysis of the long-term atmospheric CO2 concentration record of the station Point Barrow in Alaska suggests that the peak-to-peak amplitude of CO2 increased by 23 +/- 11% for a +1 degrees C anomaly in T-max from May to September over lands north of 51 degrees N, but decreased by 28 +/- 14% for a +1 degrees C anomaly in T-min. These lines of evidence suggest that asymmetric diurnal warming, a process that is currently not taken into account in many global carbon cycle models, leads to a divergent response of Northern Hemisphere vegetation growth and carbon sequestration to rising temperatures.
关键词NET PRIMARY PRODUCTIONCARBON-DIOXIDERIDGE REGRESSIONLEAF RESPIRATIONCLIMATE-CHANGESATELLITETEMPERATUREIMPACTGROWTH
语种英语
WOS研究方向Science & Technology - Other Topics
WOS类目Multidisciplinary Sciences
WOS记录号WOS:000323888300037
来源期刊NATURE
来源机构中国科学院青藏高原研究所
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/258245
推荐引用方式
GB/T 7714
Peng, Shushi,Piao, Shilong,Ciais, Philippe,et al. Asymmetric effects of daytime and night-time warming on Northern Hemisphere vegetation[J]. 中国科学院青藏高原研究所,2013,501(7465).
APA Peng, Shushi.,Piao, Shilong.,Ciais, Philippe.,Myneni, Ranga B..,Chen, Anping.,...&Zeng, Hui.(2013).Asymmetric effects of daytime and night-time warming on Northern Hemisphere vegetation.NATURE,501(7465).
MLA Peng, Shushi,et al."Asymmetric effects of daytime and night-time warming on Northern Hemisphere vegetation".NATURE 501.7465(2013).
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