树木年代学
环境科学
苏格兰松
气候变化
沙漠和干旱灌木丛
湿地
树形线条
物候学
滨海平原
自然地理学
原性土壤
气候学
松属
生态学
地理
地质学
栖息地
土壤水分
生物
土壤科学
考古
植物
作者
Alberto Arzac,Daniel Díaz-de-Quijano,Kseniia I. Khotcinskaia,Ivan Tychkov,Viktor I. Voronin,Alexander V. Kirdyanov
标识
DOI:10.1016/j.agrformet.2021.108764
摘要
• Baikal alleviates climate control in coastal sites by reducing water stress. • Simulations showed differences in the limiting factors of tree growth among sites. • The effect of climate change will not be dramatic for the coastal vegetation. Large lakes and wetlands control local and regional climate conditions. Since climate controls tree-ring formation, it is expected that air-water-land interaction at Lake Baikal region (southern Siberia), the world's largest freshwater reservoir, could potentially impact tree growth in the surrounding areas. Therefore, we aimed to determine if Lake Baikal influences Pinus sylvestris L. tree-ring growth by modifying climate conditions and alleviating climate limiting factors of tree growth in its neighboring areas. Here we combine dendrochronological measurements with tree growth modeling to evaluate the variability in the climate response of Scots pine annual (tree-ring width) and intra-annual (earlywood and latewood widths) growth and phenology at four sites (two inland and two coastal sites) in the Baikal region for the 1960–2016 period. Tree growth was significantly higher, with longer growing seasons, at the inland sites than at coastal sites. However, an increasingly negative effect of summer temperature and a positive effect of relative humidity on tree-ring growth were observed with increasing distance to the lake. The results suggest that although Lake Baikal's thermal mass lessens the climate control on the tree growth by acting as a thermal and hydric buffer in the downwind coastal sites, other factors than climate might potentially control tree growth in the region. Our results also suggest that the high plasticity of P. sylvestris to thrive in different environmental conditions will probably allow a better adaptation to the projected warmer regional climate than non-drought tolerant species inhabiting the same region.
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