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Spatial variation and temporal instability in climate-growth relationships of sessile oak (Quercus petraea [Matt.] Liebl.) under temperate conditions

机译:温带条件下无柄栎(栎属[Matt。] Liebl。)的气候-生长关系的空间变异和时间不稳定性

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Temporal instability of forest climate-growth relationships has been evidenced at high elevations and latitudes, and in Mediterranean contexts. Investigations under temperate conditions, where growth is under the control of both winter frost and summer water stress, are scarce and could provide valuable information about the ability of forest to cope with climate change. To highlight the main climatic factors driving the radial growth of Quercus petraea forests and to detect their possible evolutions over the last century, dendroecological analyses were performed along a longitudinal gradient of both decreasing summer water stress and increasing winter frost in northern France (from oceanic to semi-continental conditions). The climate-growth relationships were evaluated from 31 tree-ring chronologies (720 trees) through the calculation of moving correlation functions. Q. petraea displayed a rather low sensitivity to climate. High temperature in March and water stress from May to July appeared to be the main growth limiting factors. The sensitivity to winter precipitation and summer water stress decreased from oceanic to semi-continental conditions, whilst the correlation to winter frost tended to increase. Moving correlations revealed a general instability of climate-growth relationships, with a moderate synchronicity with climatic fluctuations. The main changes occurred during previous autumn for both temperature and precipitation whilst climatic trends were rather low or non-significant. The most coherent trends were pointed out (i) in April with a cooling (-0.9A degrees C) leading to positive correlation to temperature at the end of the century, and (ii) in July with a decreasing inter-annual variability of precipitation resulting in a loss of correlation. On the contrary, the decreasing temperature and increasing precipitation in May and June led to few significant changes climate-growth relationships.
机译:在高海拔和高纬度地区以及在地中海地区,已经证明了森林气候与生长关系的时间不稳定。在温带条件下进行的调查很少,而且在冬季霜冻和夏季水分胁迫的控制下,这种调查很少,并且可以提供有关森林应对气候变化能力的有价值的信息。为了突出驱动栎属森林径向生长的主要气候因素并检测其在上个世纪的可能演变,沿纵向梯度进行了树状生态学分析,法国北部夏季水压力减少,冬季霜冻增加(从海洋到冬季)半洲条件)。通过移动相关函数的计算,从31个树轮年表(720棵树)中评估了气候-增长关系。 Q. petraea对气候的敏感性较低。主要的生长限制因素是3月的高温和5月至7月的水分胁迫。从冬季到半大陆,对冬季降水和夏季水分胁迫的敏感性降低,而与冬季霜冻的相关性趋于增加。不断变化的相关性揭示了气候-增长关系的总体不稳定性,与气候波动具有适度的同步性。主要的变化发生在前一个秋季,既有温度也有降水,而气候趋势相当低或不明显。指出了最一致的趋势:(i)在4月降温(-0.9A摄氏度)导致本世纪末与温度呈正相关,(ii)在7月使降水的年际变化性降低导致失去相关性。相反,5月和6月的温度下降和降水增加导致气候-生长关系几乎没有重大变化。

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