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Tree spatial patterns modulate peak snow accumulation and snow disappearance

机译:树空间模式调制峰值雪积累和雪消失

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Forests and snow covered regions frequently co-occur across the northern hemisphere. In these environments, forests are structurally and spatially complex mosaics of tree neighborhoods that are intrinsically linked to ecosystem functions. Tree and canopy structures influence snow accumulation and disappearance processes through interception and radiation attenuation. However, it is unclear if spatial heterogeneity within the forest canopy induces heterogeneity in snow accumulation and persistence. We quantitatively identified different tree neighborhoods and tested the differential effects of these within-stand neighborhoods on snow processes. Neighborhood types included individual ponderosa pine (Pinus ponderosa), Douglas-fir (Pseudotsuga menziesii) and western larch (Larix occidentalis) trees, dense overstory tree clumps, openings, and regeneration patches. Intensive measurements of snow accumulation (density and depth) and persistence (disappearance date) were made within replicate neighborhoods for three years. Overall, neighborhood type and year had a significant effect on accumulation and snow disappearance. Openings were significantly different from clumps and individuals, always accumulating more snow. Openings retained snow significantly later than clumps but were not significantly different from individuals. Within the individual tree neighborhood type, a nested species effect indicated no differences in accumulation but significant differences in disappearance between deciduous and evergreen conifers, with snow persisting longer beneath deciduous western larch. Our results suggest that canopy interception is the primary mechanism driving the accumulation phase, while snow disappearance patterns are largely a consequence of spatial variation of long-wave radiation. Reducing canopy interception and longwave radiation by increasing the abundance of widely spaced single trees and small openings with silvicultural treatments should increase snow depth and duration, and thus snow water storage. Maintaining a heterogeneous canopy structure that includes tree clumps can be used to meet multiple objectives such as provision of ungulate winter range habitat, and heterogenous understory plant phenology.
机译:森林和雪覆盖的地区经常共同发生在北半球。在这些环境中,森林是在结构上和空间复杂的树形邻居马赛克,其与生态系统功能有本质上。树木和冠层结构通过截取和辐射衰减影响积雪积累和消失过程。然而,如果森林冠层内的空间异质性诱导雪积累和持久性的异质性尚不清楚。我们定量地确定了不同的树木邻居,并测试了这些内部邻居对雪过程的差异效果。邻里类型包括单独的Ponderosa Pine(Pinus Ponderosa),Douglas-FiR(Pseudotsuga Menziesii)和Western Larch(Larix Occidentalis)树,致密的夸张树丛,开口和再生补丁。在复制街区内进行了三年内的积雪(密度和深度)和持久性(消失日期)的密集测量。总体而言,邻里类型和年对积累和雪消失有重大影响。开口与团块和个人显着不同,总是积累更多的雪。开口比丛明显晚于丛,但与个体没有显着差异。在各个树邻域类型中,嵌套物种效果表明落叶和常绿针叶树在落叶和常绿针叶树之间消失的累积差异没有差异,落满了落叶西拉落后的雪。我们的研究结果表明,树冠拦截是驱动累积阶段的主要机制,而雪消失图案主要是长波辐射的空间变化的结果。通过增加大量间隔的单树和造林处理的小开口来减少冠层拦截和长波辐射应该提高雪井和持续时间,从而增加雪水储存。维持包括树丛的异质冠层结构可用于满足多种目标,例如提供悬挂冬季范围栖息地和异质林植植物候选。

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