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Transitions in high-Arctic vegetation growth patterns and ecosystem productivity tracked with automated cameras from 2000 to 2013

机译:从2000年到2013年通过自动摄像头跟踪了北极高海拔植被生长方式和生态系统生产力的转变

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摘要

Climate-induced changes in vegetation phenology at northern latitudes are still poorly understood. Continued monitoring and research are therefore needed to improve the understanding of abiotic drivers. Here we used 14 years of time lapse imagery and climate data from high-Arctic Northeast Greenland to assess the seasonal response of a dwarf shrub heath, grassland, and fen, to inter-annual variation in snow-cover, soil moisture, and air and soil temperatures. A late snow melt and start of growing season is counterbalanced by a fast greenup and a tendency to higher peak greenness values. Snow water equivalents and soil moisture explained up to 77 % of growing season duration and senescence phase, highlighting that water availability is a prominent driver in the heath site, rather than temperatures. We found a significant advance in the start of spring by 10 days and in the end of fall by 11 days, resulting in an unchanged growing season length. Vegetation greenness, derived from the imagery, was correlated to primary productivity, showing that the imagery holds valuable information on vegetation productivity.Electronic supplementary materialThe online version of this article (doi:10.1007/s13280-016-0864-8) contains supplementary material, which is available to authorized users.
机译:仍然不太了解气候引起的北纬植被物候变化。因此,需要持续的监测和研究,以增进对非生物驱动因素的理解。在这里,我们使用了高北极东北格陵兰岛14年的时间推移图像和气候数据来评估矮矮灌木丛,草地和对季节性积雪,土壤湿度和空气的年际变化的季节性响应。土壤温度。较晚的融雪和生长季节的开始被快速的绿化和较高的峰值绿色度趋势所抵消。相当于生长季节持续时间和衰老阶段的77%的雪水当量和土壤湿度可以解释,这表明水的可用性是荒地而非温度的主要驱动因素。我们发现春季开始的10天和秋季结束的11天都有明显的进步,导致生长季节的长度没有变化。从图像中得出的植被绿色度与初级生产力相关,表明该图像具有有关植被生产力的宝贵信息。电子补充材料本文的在线版本(doi:10.1007 / s13280-016-0864-8)包含补充材料,可供授权用户使用。

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