雪高传感器揭示高山草原物候变化

IF 10.8 1区 环境科学与生态学 Q1 BIODIVERSITY CONSERVATION
Michael Zehnder, Beat Pfund, Jan Svoboda, Christoph Marty, Yann Vitasse, Jake Alexander, Janneke Hille Ris Lambers, Christian Rixen
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引用次数: 0

摘要

高山地区的长期物候数据往往局限于少数几个地点,因此,对树线以上气候变化引起的植物物候变化知之甚少。由于季节性积雪地区的植物生长起始在很大程度上受融雪时间和当地温度的驱动,因此同时跟踪物候变化、融雪和近地温度是必要的。在本研究中,我们利用安装在瑞士阿尔卑斯山气候站的超声波雪高传感器,揭示了25年来(1998-2023年)草原生态系统的物候进展及其与气候变化的关系。当没有雪时,这些雪高传感器还能以独特的精细时间尺度提供植物生长信息。我们应用了两步机器学习算法来分离积雪和植物高度测量,使我们能够确定122个站点在1560到2950米之间的融化情况。,并为用于物候分析的40个站点子集提取季节性植物生长信号。我们确定了生长的开始并计算了温度趋势,特别关注熔化和生长开始之间的热条件。我们观察到,与高达+0.8°C/ 10年的强变暖相一致的是,变绿期每10年增加- 2.4天。尽管在研究期间,该重点区域的融雪时间没有显著变化,但由于光周期和热约束的不同影响,对早期融雪年的物候响应有所不同,而这些影响在不同海拔和群落中并不同等重要。因此,如果未来的融雪时间如预测的那样提前,高山草原的物候变化可能会变得更加明显。随着气候变化对山地生态系统的持续重塑,了解物候变化与物种更替之间的相互作用对于预测未来高寒地区生物多样性格局和提供保护策略至关重要。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Snow Height Sensors Reveal Phenological Advance in Alpine Grasslands

Snow Height Sensors Reveal Phenological Advance in Alpine Grasslands

Long-term phenological data in alpine regions are often limited to a few locations and thus, little is known about climate-change-induced plant phenological shifts above the treeline. Because plant growth initiation in seasonally snow-covered regions is largely driven by snowmelt timing and local temperature, it is essential to simultaneously track phenological shifts, snowmelt, and near-ground temperatures. In this study, we make use of ultrasonic snow height sensors installed at climate stations in the Swiss Alps to reveal the phenological advance of grassland ecosystems and relate them to climatic changes over 25 years (1998–2023). When snow is absent, these snow height sensors additionally provide information on plant growth at a uniquely fine temporal scale. We applied a two-step machine learning algorithm to separate snow- from plant-height measurements, allowing us to determine melt-out for 122 stations between 1560 and 2950 m a.s.l., and to extract seasonal plant growth signals for a subset of 40 stations used for phenological analyses. We identified the start of growth and calculated temperature trends, focusing particularly on thermal conditions between melt-out and growth initiation. We observed an advance of green-up by −2.4 days/decade coinciding with strong warming of up to +0.8°C/decade. Although the timing of snowmelt has not changed significantly over the study period in this focal region, phenological responses to early melt-out years varied due to differing influences of photoperiodic and thermal constraints, which were not equally important across elevations and communities. Phenological shifts of alpine grasslands are thus likely to become even more pronounced if snowmelt timing advances in the future as predicted. As climate change continues to reshape mountain ecosystems, understanding the interplay between phenological changes and species turnover will be essential for predicting future biodiversity patterns and informing conservation strategies in alpine regions.

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来源期刊
Global Change Biology
Global Change Biology 环境科学-环境科学
CiteScore
21.50
自引率
5.20%
发文量
497
审稿时长
3.3 months
期刊介绍: Global Change Biology is an environmental change journal committed to shaping the future and addressing the world's most pressing challenges, including sustainability, climate change, environmental protection, food and water safety, and global health. Dedicated to fostering a profound understanding of the impacts of global change on biological systems and offering innovative solutions, the journal publishes a diverse range of content, including primary research articles, technical advances, research reviews, reports, opinions, perspectives, commentaries, and letters. Starting with the 2024 volume, Global Change Biology will transition to an online-only format, enhancing accessibility and contributing to the evolution of scholarly communication.
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