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Annual variations in pollen deposition and meteorological conditions on the fell Aakenustunturi in northern Finland: Potential for using fossil pollen as a climate proxy

机译:芬兰北部堕落的Aakenustunturi的花粉沉积和气象条件的年度变化:使用化石花粉作为气候替代物的潜力

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摘要

Annual variation in meteorological parameters (7 years) and pollen deposition (6 years) for 4 sites on a transect across an altitudinal timberline on Aakenus, a fell in northern Finland were monitored, in order to see how pollen production, as reflected by pollen deposition (grains cm~(-2) year~(-1)), is related to climate conditions. Wind direction and wind speed before and after estimated flowering time were determined. These indicated that, within the forest and at the physiognomic forest line, pollen deposition is primarily from plants growing within the forested area on the fell and that the contribution of windblown pollen from further south is minimal. Pollen deposition can, therefore, be taken as equivalent to pollen production. Simple linear correlation coefficients between pollen deposition and one-month and two-week mean temperature, effective temperature sums and cumulative effective temperature sums for the current and previous summers were calculated.
机译:监测芬兰北部北部Aakenus一条高空林线上一条样带上4个样点的气象参数(7年)和花粉沉积(6年)的年度变化,以观察花粉沉积所反映的花粉产量(谷物厘米〜(-2)年〜(-1)),与气候条件有关。确定估计的开花时间前后的风向和风速。这些结果表明,在森林内和在自然地理学上的森林系中,花粉沉积主要来自于森林茂盛地区的植物,而来自南方的风吹花粉的贡献很小。因此,花粉沉积可以等同于花粉生产。计算了当前和以前夏季的花粉沉积与一个月和两周平均温度,有效温度总和和累积有效温度总和之间的简单线性相关系数。

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