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Timing of spring migration in birds: long-term trends, North Atlantic Oscillation and the significance of different migration routes

机译:鸟类春季迁徙的时间:长期趋势,北大西洋涛动以及不同迁徙路线的重要性

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摘要

We studied long-term trends and the yearly variation in mean spring passage time in 36 passerine bird species trapped at Ottenby Bird Observatory in south-eastern Sweden. Between the years 1952-2002, data were available for 22-45 years depending on species. Most long-distance migrant species passed progressively earlier over the study period (range: 2.5 days earlier to 0.7 days later per 10 years, with an average of 0.9 days earlier per 10 years). The annual variation in timing of migration in most species, regardless of migration distance, correlated negatively with the winter index of the North Atlantic Oscillation (NAO), a large-scale climate phenomenon influencing the climate in the North Atlantic region. Birds passed earlier after mild and humid winters., corresponding to the high phase of the NAO. This corroborates the pattern round at a nearby migration site with a comparable dataset (Helgoland, 600 km WSW of Ottenby). However, short/medium-distance migrant species at Otterby, in contrast to the situation at Helgoland, have shown no general trend of earlier passage in recent years. This was probably a consequence of the shorter study period at Ottenby, which included only the last 22-32 years (41 years at Helgoland), when the NAO showed no significant trend. At the species-specific level, the long-term trends in passage time were similar at the two sites, and there was some congruence to the extent that a given species was affected by NAO. Long-distance migrants wintering south and south-east of the breeding grounds showed some of the strongest changes in long-term trends (passing progressively earlier) at Ottenby, and for some of these species passage time varied negatively with NAO. Obviously, and contrary to previous suggestions, variations in NAO also influence birds migrating through eastern Europe, although the direct or indirect mechanisms through which this is achieved are unknown.
机译:我们研究了瑞典东南部奥滕比鸟类天文台捕获的36种雀形目鸟类的长期趋势和平均春季通过时间的年变化。在1952年至2002年之间,根据物种,可获得22至45年的数据。在研究期间,大多数长途迁徙物种逐渐通过(范围:每10年提前2.5天到晚0.7天,平均每10年提前0.9天)。大多数物种的迁徙时间每年变化,无论迁徙距离如何,都与北大西洋涛动(NAO)的冬季指数负相关,北大西洋涛动(NAO)的冬季指数影响北大西洋区域的气候。冬季温和潮湿之后,鸟类通过得更早,这与NAO的高阶段相对应。这可以用可比较的数据集(Helgoland,奥特比西WSW 600公里)证实在附近的迁移地点进行的模式回合。但是,与黑尔戈兰群岛的情况相比,奥特比的中短距离迁徙物种近年来没有显示出较早通过的总体趋势。这可能是Ottenby研究期较短的结果,该研究期仅包括最近的22-32年(Helgoland为41年),而NAO没有显示出明显的趋势。在物种特定的水平上,两个地方的通过时间的长期趋势是相似的,并且在给定物种受NAO影响的程度上存在一定的一致性。在繁殖场南部和东南部越冬的长途迁徙者在奥滕比的长期趋势中显示出一些最强烈的变化(逐渐越早越过),并且对于其中一些物种,传播时间与NAO呈负相关。显然,与先前的建议相反,NAO的变化也影响通过东欧迁移的鸟类,尽管实现这一目标的直接或间接机制尚不清楚。

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