Department of Geography, University of Colorado, 260 UCB, Boulder, Colorado, 80302, USA.
Institute of Arctic and Alpine Research, University of Colorado, 1560 30th Street, Boulder, Colorado, 80303, USA.
Ecology. 2017 Oct;98(10):2698-2707. doi: 10.1002/ecy.1963.
This study used Landsat-based detection of spruce beetle (Dendroctonus rufipennis) outbreak over the years 2000-2014 across the Southern Rocky Mountain Ecoregion to examine the spatiotemporal patterns of outbreak and assess the influence of temperature, drought, forest characteristics, and previous spruce beetle activity on outbreak development. During the 1999-2013 period, time series of spruce beetle activity were highly spatially correlated (r > 0.5) at distances <5 km, but remained weakly correlated (r = 0.08) at distances >400 km. Furthermore, cluster analysis on time series of outbreak activity revealed the outbreak developed at multiple incipient locations and spread to unaffected forest, highlighting the importance of both local-scale dispersal and regional-scale drivers in synchronizing spruce beetle outbreak. Spatial overlay analysis and Random Forest modeling of outbreak development show that outbreaks initiate in areas characterized by summer, winter, and multi-year drought and that outbreak spread is strongly linked to the proximity and extent of nearby outbreak, but remains associated with drought. Notably, we find that spruce beetle outbreak is associated with low peak snow water equivalent, not just summer drought. As such, future alterations to both winter and summer precipitation regimes are likely to drive important changes in subalpine forests.
本研究利用 2000 年至 2014 年期间南方落矶山脉生态区基于 Landsat 的云杉甲虫(Dendroctonus rufipennis)爆发检测,以研究爆发的时空模式,并评估温度、干旱、森林特征以及先前云杉甲虫活动对爆发发展的影响。在 1999 年至 2013 年期间,云杉甲虫活动的时间序列在小于 5 公里的距离内具有高度的空间相关性(r>0.5),但在大于 400 公里的距离内相关性较弱(r=0.08)。此外,对爆发活动时间序列的聚类分析表明,爆发是在多个初始地点发生的,并蔓延到未受影响的森林,这突显了局部尺度扩散和区域尺度驱动因素在协调云杉甲虫爆发方面的重要性。爆发发展的空间叠加分析和随机森林模型表明,爆发发生在夏季、冬季和多年干旱特征的区域,爆发的蔓延与附近爆发的接近程度和范围密切相关,但仍与干旱有关。值得注意的是,我们发现云杉甲虫爆发与低峰值雪水当量有关,而不仅仅是夏季干旱。因此,未来冬季和夏季降水模式的变化可能会导致亚高山森林发生重要变化。