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首页> 外文期刊>Global change biology >A model-data comparison of Holocene timberline changes in the Swiss Alps reveals past and future drivers of mountain forest dynamics.
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A model-data comparison of Holocene timberline changes in the Swiss Alps reveals past and future drivers of mountain forest dynamics.

机译:瑞士阿尔卑斯山全新世林线变化的模型数据比较揭示了过去和未来山地森林动态的驱动力。

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Mountain vegetation is strongly affected by temperature and is expected to shift upwards with climate change. Dynamic vegetation models are often used to assess the impact of climate on vegetation and model output can be compared with paleobotanical data as a reality check. Recent paleoecological studies have revealed regional variation in the upward shift of timberlines in the Northern and Central European Alps in response to rapid warming at the Younger Dryas/Preboreal transition ca. 11 700 years ago, probably caused by a climatic gradient across the Alps. This contrasts with previous studies that successfully simulated the early Holocene afforestation in the (warmer) Central Alps with a chironomid-inferred temperature reconstruction from the (colder) Northern Alps. We use LandClim, a dynamic landscape vegetation model to simulate mountain forests under different temperature, soil and precipitation scenarios around Iffigsee (2065 m a.s.l.) a lake in the Northwestern Swiss Alps, and compare the model output with the paleobotanical records. The model clearly overestimates the upward shift of timberline in a climate scenario that applies chironomid-inferred July-temperature anomalies to all months. However, forest establishment at 9800 cal. BP at Iffigsee is successfully simulated with lower moisture availability and monthly temperatures corrected for stronger seasonality during the early Holocene. The model-data comparison reveals a contraction in the realized niche of Abies alba due to the prominent role of anthropogenic disturbance after ca. 5000 cal. BP, which has important implications for species distribution models (SDMs) that rely on equilibrium with climate and niche stability. Under future climate projections, LandClim indicates a rapid upward shift of mountain vegetation belts by ca. 500 m and treeline positions of ca. 2500 m a.s.l. by the end of this century. Resulting biodiversity losses in the alpine vegetation belt might be mitigated with low-impact pastoralism to preserve species-rich alpine meadows.
机译:山区植被受到温度的强烈影响,预计会随着气候变化而向上移动。动态植被模型通常用于评估气候对植被的影响,并且可以将模型输出与古植物数据进行比较,以进行实际检查。近期的古生态学研究表明,北欧和中欧阿尔卑斯山林线向上移动的区域性变化是由于约克·德里亚斯/早原地带过渡时期迅速变暖所致。 11700年前,可能是由于阿尔卑斯山的气候梯度造成的。这与以前的研究形成对比,之前的研究成功地通过(冷)北阿尔卑斯山进行了天文学家推断的温度重建,成功地模拟了(较暖)中阿尔卑斯山的早期全新世造林。我们使用LandClim这个动态景观植被模型来模拟瑞士西北阿尔卑斯山的Iffigsee(2065 m a.s.l.)湖周围不同温度,土壤和降水情景下的山地森林,并将模型输出与古植物记录进行比较。该模型明显高估了在气候情境中林线的向上移动,这种气候情境适用了由推断的7月温度异常到所有月份。但是,森林建立在9800 cal。成功地模拟了Iffigsee的BP,其较低的水分供应量和每月温度已得到校正,从而在全新世早期具有较强的季节性。模型数据的比较表明,由于人为干扰的显着作用,大约在Abies alba的已实现生态位中出现了收缩。 5000卡路里BP对依赖于气候和生态位稳定的平衡的物种分布模型(SDM)具有重要意义。在未来的气候预测下,LandClim表示山地植被带迅速向上移动了大约1个百分点。 500 m和大约的树线位置。 2500立方米到本世纪末。可以通过低影响的放牧来减轻高山植被带中生物多样性的丧失,以保护物种丰富的高山草甸。

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