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Contrasting effects of wildfire and climate on radial growth of Pinus canariensis on windward and leeward slopes on Tenerife, Canary Islands

机译:野火和气候对加那利群岛特内里费岛上风和下风斜坡上加拿大松松径向生长的影响

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摘要

Little is known concerning the effects of wildfires on tree radial growth and their climatic response under contrasting regimes of fog water inputs on oceanic islands. On Tenerife, Canary Islands, windward slopes are humid with high-fog frequency due to influence of wet trade winds, while climate on leeward slopes is more arid. We used tree-ring records of Pinus canariensis Sweet ex Spreng. to quantify the effects of a fire of known date on radial growth and determine the main limiting climatic factors for growth. Radial growth patterns and their responsiveness to fire severity and climatic variation differed between windward and leeward slopes. Surface fire did not significantly impact growth, while crown fire caused short-term growth reduction, and even cessation, more pronounced on the windward slope. Growth rates, tree-ring common signal, and climate sensitivity were smaller on the windward slope, with cold winters, and summer water stress limiting growth. On the leeward slope, climate explained a greater amount of growth variation mainly due to negative effects of high October-December sea-level pressures causing dry winter conditions. Contrasting growth dynamics on both slopes may result from diverging physiological effects of water inputs and reduced radiation caused by fog drip. Our findings suggest that dating growth suppressions and absent rings are useful to date past high-severity crown fires in P. canariensis forests, in addition to ordinary fire scars dating indicative of low-severity surface fires. © 2011 Springer-Verlag.
机译:关于野火对大洋岛屿上雾水输入的对比情况下树木径向生长及其对气候响应的影响知之甚少。在加那利群岛的特内里费岛,由于潮湿的商风的影响,迎风坡的湿度较高,雾气频率较高,而背风坡的气候更为干旱。我们使用了加拿大松(Pinus canariensis)Sweet ex Spreng的年轮记录。量化已知日期火灾对径向生长的影响,并确定生长的主要限制气候因素。迎风坡和背风坡的径向生长方式及其对火灾严重性和气候变化的响应程度有所不同。地表火并没有显着影响生长,而树冠火则导致短期生长减少甚至停止,在迎风坡上更为明显。在迎风坡上,生长速度,树木年轮共同信号和气候敏感性较小,冬季寒冷,夏季水分胁迫限制了生长。在背风坡上,气候解释了较大的增长变化,这主要是由于10月至12月海平面高压力造成了干燥的冬季条件。两个斜坡上不同的生长动力学可能是由于水输入的生理效应不同以及由于雾滴引起的辐射减少所致。我们的发现表明,除了普通的火伤痕迹表明低烈度地表火的年代外,约会生长抑制和无环的约会对于过去的高加那利森林高烈度冠火是有用的。 ©2011年Springer-Verlag。

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