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秋尺蠖/冬尺蠖爆发中的波动与同步性。II. 太阳黑子活动无法解释周期性爆发。

Waves and synchrony in Epirrita autumnata/Operophtera brumata outbreaks. II. Sunspot activity cannot explain cyclic outbreaks.

作者信息

Nilssen A C, Tenow O, Bylund H

机构信息

Zoology Department, Tromsø Museum, University of Tromsø, Tromsø, Norway.

出版信息

J Anim Ecol. 2007 Mar;76(2):269-75. doi: 10.1111/j.1365-2656.2006.01205.x.

Abstract
  1. In recent studies, it has been argued that sunspot activity forces the Epirrita autumnata 9-10-year outbreak periodicity in the mountain birch forest of Fennoscandia. For the following reasons, we challenge this conclusion. 2. With a 10-year outbreak cycle of E. autumnata and the 11-year sunspot cycle, it is expected that the cycles will run in-phase, out-of-phase and in-phase within 10 x 11 years. Hence, given such cycle lengths, sunspot activity should not affect outbreak periods. For a test, the E. autumnata series should be at least 110 years in length. 3. A well-documented E. autumnata outbreak series of 81 years (1888-1968; outbreak periods IV-XII) exists. This series is here lengthened to 114 years by adding outbreak frequencies for three decades (1969-2001). 4. By lengthening the series, three more E. autumnata/Operophtera brumata periods (XIII, XIV, XV) are identified. Period XV, like several earlier periods, was of the moving type, i.e. outbreaks moved in a wavelike manner from northern Fennoscandia to southern Norway. 5. As with several earlier outbreak periods in central northern Fennoscandia, the main timing of periods XIII-XV centred at the middle of the decades. In contrast, outbreaks at the extreme north-western coast of Norway centred at the decadal shifts, i.e. about 1979, 1989 and 1999. Supported by historical documents, we explain the 1979 and 1999 outbreaks as the final expressions of east-west outbreak waves that branched off from the main waves which moved southward during periods XIII and XV. These side-waves in the north are new observations. Outbreaks at the decadal shift 1989/1990 may have been of a more complex nature. 6. We find that sunspot activity does not explain outbreak waves. Furthermore, a test of our 114-year long E. autumnata series against the contemporaneous sunspot series shows that the two series run in-phase and out-of-phase. The observed interval between the two cycles coming in-phase agrees with the expected interval. This challenges the hypothesis of sunspot synchronization of the E. autumnata (and O. brumata) outbreaks.
摘要
  1. 在最近的研究中,有人认为太阳黑子活动导致了芬诺斯堪的亚山区桦树林中Epirrita autumnata的9至10年爆发周期。基于以下原因,我们对这一结论提出质疑。2. 鉴于Epirrita autumnata的爆发周期为10年,太阳黑子周期为11年,预计这两个周期将在10×11年内同相、异相和同相运行。因此,考虑到这样的周期长度,太阳黑子活动不应影响爆发周期。为了进行检验,Epirrita autumnata系列至少应有110年的长度。3. 存在一个有充分记录的81年(1888 - 1968年;爆发周期IV - XII)的Epirrita autumnata爆发系列。通过添加三个十年(1969 - 2001年)的爆发频率,这个系列在此被延长至114年。4. 通过延长该系列,又确定了另外三个Epirrita autumnata/Operophtera brumata周期(XIII、XIV、XV)。与几个早期周期一样,周期XV是移动型的,即爆发以波浪状从芬诺斯堪的亚北部向挪威南部移动。5. 与芬诺斯堪的亚中北部几个早期爆发周期一样,周期XIII - XV的主要时间集中在几十年的中间。相比之下,挪威西北海岸极端地区的爆发集中在年代交替时,即大约1979年、1989年和1999年。在历史文献的支持下,我们将1979年和1999年的爆发解释为在周期XIII和XV期间向南移动的主波分支出来的东西向爆发波的最终表现。北部的这些侧波是新的观测结果。1989/1990年代交替时的爆发可能具有更复杂的性质。6. 我们发现太阳黑子活动无法解释爆发波。此外,将我们114年长的Epirrita autumnata系列与同期太阳黑子系列进行检验表明,这两个系列同相和异相运行。观测到的两个周期同相的间隔与预期间隔一致。这对Epirrita autumnata(和Operophtera brumata)爆发的太阳黑子同步假说提出了挑战。

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