Tree ring delta O-18 reveals no long-term change of atmospheric water demand since 1800 in the northern Great Hinggan Mountains, China

Global warming will significantly increase transpirational water demand, which could dramatically affect plant physiology and carbon and water budgets. Tree ring delta O-18 is a potential index of the leaf-to-air vapor-pressure deficit (VPD) and therefore has great potential for long-term climatic r...

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Bibliographic Details
Published in:Journal of Geophysical Research: Atmospheres
Main Authors: Liu, Xiaohong, Zhang, Xuanwen, Zhao, Liangju, Xu, Guobao, Wang, Lixin, Sun, Weizhen, Zhang, Qiuliang, Wang, Wenzhi, Zeng, Xiaomin, Wu, Guoju
Format: Article in Journal/Newspaper
Language:English
Published: AMER GEOPHYSICAL UNION 2017
Subjects:
Science & Technology
Physical Sciences
Meteorology & Atmospheric Sciences
OXYGEN-ISOTOPE RATIOS
VAPOR-PRESSURE DEFICIT
STABLE-ISOTOPES
MODERN PRECIPITATION
NORTHWESTERN CHINA
TIBETAN PLATEAU
FOREST
CLIMATE
TEMPERATURE
CELLULOSE
permafrost
Online Access:http://ir.imde.ac.cn/handle/131551/19038
https://doi.org/10.1002/2017JD026660
Description
Summary:Global warming will significantly increase transpirational water demand, which could dramatically affect plant physiology and carbon and water budgets. Tree ring delta O-18 is a potential index of the leaf-to-air vapor-pressure deficit (VPD) and therefore has great potential for long-term climatic reconstruction. Here we developed delta O-18 chronologies of two dominant native trees, Dahurian larch (Larix gmelinii Rupr.) and Mongolian pine (Pinus sylvestris var. mongolica), from a permafrost region in the Great Hinggan Mountains of northeastern China. We found that the July-August VPD and relative humidity were the dominant factors that controlled tree ring delta O-18 in the study region, indicating strong regulation of stomatal conductance. Based on the larch and pine tree ring delta O-18 chronologies, we developed a reliable summer (July-August) VPD reconstruction since 1800. Warming growing season temperatures increase transpiration and enrich cellulose O-18, but precipitation seemed to be the most important influence on VPD changes in this cold region. Periods with stronger transpirational demand occurred around the 1850s, from 1914 to 1925, and from 2005 to 2010. However, we found no overall long-term increasing or decreasing trends for VPD since 1800, suggesting that despite the increasing temperatures and thawing permafrost throughout the region, forest transpirational demand has not increased significantly during the past two centuries. Under current climatic conditions, VPD did not limit growth of larch and pine, even during extremely drought years. Our findings will support more realistic evaluations and reliable predictions of the potential influences of ongoing climatic change on carbon and water cycles and on forest dynamics in permafrost regions.

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