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A late Holocene record of solar-forced atmospheric blocking variability over Northern Europe inferred from varved lake sediments of Lake Kuninkaisenlampi

机译:从古尼凯森兰皮湖的湖泊沉积物中推断出的全新世晚期北欧强迫的大气阻塞变化的记录

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This study presents a new varved lake sediment sequence from Lake Kuninkaisenlampi, Eastern Finland. The record is constituted by alternations of clastic and biogenic laminae and provides a precise chronology extending back to 3607 +/- 94 varve yrs. BP. The seasonality of the boreal climatic zone, with cold winters and mild summers, is reflected in the varve structure as a succession of three laminae from bottom to top, (i) a coarse to fine-grained detrital lamina marked by detrital catchment material transported by spring floods; (ii) a biogenic lamina with diatoms, plant and insect remnants reflecting biological productivity during the season of lake productivity; and (iii) a very fine amorphous organic lamina deposited during the winter stratification. The thickness of the detrital lamina in the lake reflects changes in the rate of spring snow melt in the catchment and is, therefore, considered a proxy for winter conditions. Hence, the record allows reconstructing local climate and environmental conditions on inter annual to the multi-centennial timescales. We find that minerogenic accumulation reflected in the detrital lamina exhibits a high multi-decadal to centennial-scale spectral coherency with proxies for solar activity, such as Alt, and Total Solar Irradiance, suggesting a strong link between solar variability and sediment transport to the lake basin. Increased catchment erosion is observed during periods of low solar activity, which we ascribe to the development of more frequent atmospheric winter blocking circulation induced by solar-forced changes in the stratosphere. We suggest that soil frost in the catchment of Lake Kuninkaisenlampi related to more frequent winter blocking led to increased surface run-off and ultimately to increased catchment erosion during spring. We conclude that, during the past ca 3600 years, solar forcing may have modulated multi-decadal to centennial variations in sedimentation regimes in lakes from Eastern Finland and potentially in other North European lakes. (C) 2016 Elsevier Ltd. All rights reserved.
机译:这项研究提出了来自芬兰东部的Kuninkaisenlampi湖的新的脉状湖泊沉积物序列。该记录由碎屑和生物成因层片交替组成,并提供了精确的年代顺序,可以追溯到3607 +/- 94 varve yrs。 BP。脉管结构反映了北部气候区的季节性,冬季寒冷而夏季温和,从底部到顶部依次是三个薄片,(i)粗粒至细粒的碎屑层,其特征是由春季洪水; (ii)具有硅藻,植物和昆虫残留物的生物薄片,反映了湖泊生产力季节的生物生产力; (iii)在冬季分层过程中沉积的非常细的非晶态有机薄层。湖中碎屑层的厚度反映了集水区春季融雪速率的变化,因此被认为是冬季条件的替代。因此,该记录允许在每年至多百年的时间尺度上重建当地的气候和环境条件。我们发现,碎屑层中反映的成矿累积表现出很高的年代际至百年尺度尺度的光谱一致性,并且具有太阳活动的代理,例如Alt和总太阳辐照度,这表明太阳变异性与沉积物向湖的输送之间有很强的联系。盆地。在低太阳活动期间观测到流域侵蚀增加,这归因于平流层中太阳强迫变化引起的更频繁的大气冬季阻塞循环的发展。我们认为,Kuninkaisenlampi湖流域的土壤霜冻与更频繁的冬季阻塞有关,导致地表径流增加,并最终导致春季流域侵蚀增加。我们得出的结论是,在过去大约3600年中,日光强迫可能已调节了芬兰东部湖泊以及其他北欧湖泊中沉积机制的年代际变化至百年变化。 (C)2016 Elsevier Ltd.保留所有权利。

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