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Spatiotemporal variations of alpine climate, snow cover and phenology

机译:高山气候,雪覆盖和候选的时空变化

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Understanding the relationships between vegetation phenology and its seasonal drivers under varying site conditions is of high interest in mountain areas, since alpine ecosystems are assumed to be particularly sensitive to climatic changes. Through the joint analysis of NDVI, snow metrics, and climate data at 250 m and 2 km spatial resolution, respectively, we aim at identifying their temporal and spatial variability and statistical inter- and intra-annual relationships on an alpine-wide scale. Apart from clear patterns in the vegetation and snow metrics related to topography, a negative relationship of mean March NDVI to snow cover duration (SCD) in the preceding months was detected, indicating a high sensitivity of green-up to snow accumulation and melt. In contrast, positive correlations between early winter SCDs and late summer NDVI indicate a lagged water storage effect. On the local scale of South Tyrol, climate variability interacted with topography could explain on average 30% of NDVI variations from late-October till late-May.
机译:了解植被候选的关系及其在不同现场条件下的季节性司机在山区的高度兴趣,因为Alpine生态系统被认为对气候变化特别敏感。通过在250米和2公里的空间分辨率下的NDVI,雪指标和气候数据的联合分析,我们的目的是在高山范围内识别他们的时间和空间变异性和统计间关系和统计间关系。除了与地形相关的植被和雪指标中的明确模式,检测到前几个月的平均3月NDVI与雪覆盖持续时间(SCD)的负面关系,表明绿色膨胀和熔化的高敏感性。相比之下,冬季冬季SCDS和晚夏季NDVI之间的正相关性表示滞后的蓄水效果。在南蒂罗尔的局部规模上,与地形相互作用的气候变异可以平均解释10月晚上至5月晚期的30%的NDVI变化。

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