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Variability and evolution of global land surface phenology over the past three decades (1982-2012)

机译:过去三十年(1982年至2012年)全球陆地表面物候的变化和演变

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Monitoring land surface phenology (LSP) is important for understanding both the responses and feedbacks of ecosystems to the climate system, and for representing these accurately in terrestrial biosphere models. Moreover, by shedding light on phenological trends at a variety of scales, LSP provides the potential to fill the gap between traditional phenological (field) observations and the large-scale view of global models. In this study, we review and evaluate the variability and evolution of satellite-derived growing season length (GSL) globally and over the past three decades. We used the longest continuous record of Normalized Difference Vegetation Index data available to date at global scale to derive LSP metrics consistently over all vegetated land areas and for the period 1982-2012. We tested GSL, start- and end-of-season metrics (SOS and EOS, respectively) for linear trends as well as for significant trend shifts over the study period. We evaluated trends using global environmental stratification information in place of commonly used land cover maps to avoid circular findings. Our results confirmed an average lengthening of the growing season globally during 1982-2012 - averaging 0.22-0.34daysyr(-1), but with spatially heterogeneous trends. About 13-19% of global land areas displayed significant GSL change, and over 30% of trends occurred in the boreal/alpine biome of the Northern Hemisphere, which showed diverging GSL evolution over the past three decades. Within this biome, the Cold and Mesic' environmental zone appeared as an LSP change hotspot. We also examined the relative contribution of SOS and EOS to the overall changes, finding that EOS trends were generally stronger and more prevalent than SOS trends. These findings constitute a step towards the identification of large-scale phenological drivers of vegetated land surfaces, necessary for improving phenological representation in terrestrial biosphere models.
机译:监测地表物候(LSP)对于理解生态系统对气候系统的响应和反馈以及在陆地生物圈模型中准确表示这些响应非常重要。此外,通过揭示各种尺度上的物候趋势,LSP提供了填补传统物候(实地)观察与全局模型大规模视图之间的空白的潜力。在这项研究中,我们回顾并评估了全球以及过去三十年中卫星衍生的生长季长度(GSL)的变异性和演变。我们使用迄今为止在全球范围内可获得的最长的归一化植被指数数据的连续记录,来得出1982-2012年期间所有植被土地面积上的LSP指标。我们针对研究期间的线性趋势以及显着趋势变化,测试了GSL,季节开始和结束时的指标(分别为SOS和EOS)。我们使用全球环境分层信息代替了常用的土地覆盖图来评估趋势,从而避免出现圆形结果。我们的结果证实了1982-2012年间全球生长季节的平均延长-平均为0.22-0.34daysyr(-1),但具有空间异质性趋势。全球约有13-19%的土地表现出GSL的显着变化,并且超过30%的趋势发生在北半球的寒带/高山生物区系中,这表明在过去的30年中,GSL的发展趋势各不相同。在这个生物群落中,“寒冷和混乱”的环境带出现为LSP变化热点。我们还检查了SOS和EOS对总体变化的相对贡献,发现EOS趋势通常比SOS趋势更强,更普遍。这些发现构成了朝着识别植被地面的大规模物候动因迈出的一步,这是改善陆地生物圈模型中物候表征的必要条件。

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