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Disentangling Contributions of CO 2 Concentration and Climate to Changes in Intrinsic Water-Use Efficiency in the Arid Boreal Forest in China’s Altay Mountains

机译:中国阿尔泰山区干旱北方森林森林中CO 2浓度和气候对内在水分利用效率变化的诱人贡献

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Intrinsic water-use efficiency ( iWUE ) is affected by the balance of photosynthetic rate, stomatal conductance, and climate, along with many other exogenous factors, such as the CO 2 concentration in the atmosphere (CO 2atm ), nutrients, and water holding capacity of the soil. The relative contributions of CO 2atm and climate to iWUE are still incompletely understood, particularly for boreal forests where the climate is undergoing unprecedented warming. We combined δ 13 C and δ 18 O in tree rings from the Siberian larch ( Larix sibirica Ledeb.) in Northwestern China’s Altay Mountains, which receives 190 mm in annual precipitation, to detect the drivers of long-term iWUE changes and their time-varying contributions over the past 222 years. A climate optimization approach was used to isolate the influence of climate from CO 2atm influence on iWUE . We found that iWUE increased about 33.6% from 1790 to 2011, and rising CO 2atm contributed 48.8% to this iWUE increase. The contributions of CO 2atm and climate (drought conditions) varied during the study period 1790–2011. From 1790 to 1876, the climate was the most important factor contributing to the changes in iWUE . From 1877 to 1972, CO 2atm was the main contributor; however, after 1973, the climate was again the dominant contributor to the increase in iWUE , especially during 1996–2011. During the period 1996–2011, climate substantially (83%) contributed to the iWUE increase. Our findings imply that, in the boreal forest in Northwestern China’s arid region, iWUE experienced three changes: (1) the climate dominating from 1790 to 1876; (2) CO 2atm dominating from 1877 to 1972, and (3) climate dominating again during the past four decades. We observed that the relationships between iWUE and tree-ring width shifted from positive to negative from 1996 onwards. These relationship changes indicate that CO 2atm -mediated effects of increasing iWUE on tree growth are counteracted by climatic drought stress and iWUE increase cannot counter the stress from drought on tree growth in China’s arid boreal forest.
机译:内在用水效率(iWUE)受光合作用,气孔导度和气候以及其他许多外源因素(例如大气中的CO 2浓度(CO 2atm),养分和持水量)的平衡的影响。的土壤。仍然没有完全了解CO 2 atm和气候对iWUE的相对贡献,特别是对于气候正在经历前所未有的变暖的北方森林。我们结合了西北阿尔伯特山西伯利亚落叶松(Larix sibirica Ledeb。)的年轮中的δ13 C和δ18 O,以检测iWUE长期变化的驱动力及其时间,该年降水量为190 mm。在过去的222年中有不同的贡献。气候优化方法用于隔离气候和CO 2 atm对iWUE的影响。我们发现,从1790年到2011年,iWUE增长了约33.6%,CO 2 atm的上升为iWUE增长贡献了48.8%。在研究期间1790-2011年,CO 2 atm和气候(干旱条件)的贡献有所不同。从1790年到1876年,气候是导致iWUE变化的最重要因素。从1877年到1972年,CO 2atm是主要贡献者。然而,在1973年之后,气候再次成为iWUE增长的主要因素,尤其是在1996-2011年期间。在1996年至2011年期间,气候(83%)大大促进了iWUE的增长。我们的发现表明,在西北干旱地区的北方森林中,iWUE经历了三个变化:(1)1790年至1876年的气候占主导地位; (2)从1877年到1972年,CO 2atm占主导地位;(3)在过去的40年中,气候再次占主导地位。我们观察到iWUE与树轮宽度之间的关系从1996年开始从正变到负。这些关系的变化表明,气候干旱胁迫可以抵消iWUE增加对树木生长的CO 2 atm介导作用,而iWUE的增加不能抵消干旱干旱对中国干旱北方森林树木生长造成的压力。

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