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Declines in northern forest tree growth following snowpack decline and soil freezing

机译:在积雪下降和土壤冻结之后,北部森林树增长下降

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摘要

Changes in growing season climate are often the foci of research exploring forest response to climate change. By contrast, little is known about tree growth response to projected declines in winter snowpack and increases in soil freezing in seasonally snow-covered forest ecosystems, despite extensive documentation of the importance of winter climate in mediating ecological processes. We conducted a 5-year snow-removal experiment whereby snow was removed for the first 4-5 weeks of winter in a northern hardwood forest at the Hubbard Brook Experimental Forest in New Hampshire, USA. Our results indicate that adverse impacts of reduced snowpack and increased soil freezing on the physiology of Acer saccharum (sugar maple), a dominant species across northern temperate forests, are accompanied by a 40 +/- 3% reduction in aboveground woody biomass increment, averaged across the 6 years following the start of the experiment. Further, we find no indication of growth recovery 1 year after cessation of the experiment. Based on these findings, we integrate spatial modeling of snowpack depth with forest inventory data to develop a spatially explicit, regional-scale assessment of the vulnerability of forest aboveground growth to projected declines in snowpack depth and increased soil frost. These analyses indicate that nearly 65% of sugar maple basal area in the northeastern United States resides in areas that typically experience insulating snowpack. However, under the RCP 4.5 and 8.5 emissions scenarios, we project a 49%-95% reduction in forest area experiencing insulating snowpack by the year 2099 in the northeastern United States, leaving large areas of northern forest vulnerable to these changes in winter climate, particularly along the northern edge of the region. Our study demonstrates that research focusing on growing season climate alone overestimates the stimulatory effect of warming temperatures on tree and forest growth in seasonally snow-covered forests.
机译:生长季节气候的变化往往是探索森林对气候变化的森林反应的焦点。相比之下,尽管在调解生态过程中的重要性广泛记录了冬季气候在调解生态过程中的重要性,但在冬季积雪中,冬季积雪的冬季积雪和土壤冻结的土壤冻结的土壤冻结了几乎没有。我们进行了一个5年的冰雪去除实验,即在美国新罕布什尔州新罕布什尔州的北硬木森林中冬季冬季的前4-5周脱落。我们的研究结果表明,减少积雪和冻结土壤冻结的土壤(北方温带森林血液污染的占优势物种的恶性的不利影响伴随着低于地上木质生物量增量的40 +/- 3%,平均在实验开始后的6年里。此外,我们发现在停止实验后1年内没有增长回收。基于这些调查结果,我们将积雪深度与森林库存数据集成了空间建模,以开发对森林脆弱性的空间明确,区域规模评估地上增长的脆弱性,以投射积雪深度和土壤霜的增加。这些分析表明,美国东北部的近65%的糖枫枫基面积居住在通常经历绝缘积雪的地区。然而,根据RCP 4.5和8.5的排放情景,我们在美国东北部门的2099年,森林面积减少49%-95%,在美国东北部门,北方森林大面积易受这些变化的冬季气候,特别是沿着该地区的北边缘。我们的研究表明,重点关注生长季节气候的研究单独高估季节性冰雪覆盖森林中变暖温度对树木和森林生长的刺激作用。

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