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Linking atmospheric terrestrial and aquatic environments: Regime shifts in the Estonian climate over the past 50 years

机译:连接大气陆地和水生环境:过去50年爱沙尼亚气候的体制变化

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摘要

Climate change in recent decades has been identified as a significant threat to natural environments and human wellbeing. This is because some of the contemporary changes to climate are abrupt and result in persistent changes in the state of natural systems; so called regime shifts (RS). This study aimed to detect and analyse the timing and strength of RS in Estonian climate at the half-century scale (1966−2013). We demonstrate that the extensive winter warming of the Northern Hemisphere in the late 1980s was represented in atmospheric, terrestrial, freshwater and marine systems to an extent not observed before or after the event within the studied time series. In 1989, abiotic variables displayed statistically significant regime shifts in atmospheric, river and marine systems, but not in lake and bog systems. This was followed by regime shifts in the biotic time series of bogs and marine ecosystems in 1990. However, many biotic time series lacked regime shifts, or the shifts were uncoupled from large-scale atmospheric circulation. We suggest that the latter is possibly due to complex and temporally variable interactions between abiotic and biotic elements with ecosystem properties buffering biotic responses to climate change signals, as well as being affected by concurrent anthropogenic impacts on natural environments.
机译:近几十年来,气候变化已被确认为对自然环境和人类福祉的重大威胁。这是因为当代的某些气候变化是突然的,并导致自然系统状态的持续变化。所谓的政权转移(RS)。这项研究旨在检测和分析半个世纪(1966-2013年)爱沙尼亚气候中RS的时间和强度。我们证明,在研究时间序列内,事件发生前后未观测到的大气,陆地,淡水和海洋系统代表了北半球1980年代后期广泛的冬季变暖。 1989年,非生物变量在大气,河流和海洋系统中显示出统计上显着的状态变化,但在湖泊和沼泽系统中则没有。随后是1990年沼泽和海洋生态系统生物时间序列的状态变化。但是,许多生物时间序列缺乏系统状态变化,或者这些变化与大规模大气环流无关。我们认为,后者可能是由于非生物和生物元素之间具有复杂且随时间变化的相互作用,具有生态系统特性,缓冲了生物对气候变化信号的响应,并且受到人为因素对自然环境的影响。

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