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Reprint of “Atlantic Multidecadal Oscillation (AMO) modulates dynamics of small pelagic fishes and ecosystem regime shifts in the eastern North and Central Atlantic”

机译:重印“大西洋多年代际涛动(AMO)调节北部中东部和大西洋中部小型中上层鱼类的动态和生态系统的变化”

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摘要

Dynamics of abundance and migrations of populations of small pelagic clupeoid fish such as anchovy (Engraulis encrasicolus), sardine (Sardina pilchardus), sardinella (Sardinella aurita), sprat (Sprattus sprattus) and herring (Clupea harengus) in the eastern North and Central Atlantic between Senegal and Norway vary in synchrony with the warm and cool phases of the Atlantic Multidecadal Oscillation (AMO). This is shown by compiling retrospective data on fish catches and anecdotal observations, which in some cases date back to the mid-19th century. The AMO is defined as the de-trended mean of North Atlantic (0-60 degrees N) sea surface temperature anomalies. However, it is not primarily the temperature which drives the dynamics of the small pelagic fish populations. Instead, the AMO seems to be a proxy for complex processes in the coupled atmosphere-ocean system of the North Atlantic. This is manifested in large-scale changes in strength and direction of the current system that move water masses around the North Atlantic and likely involves the North Atlantic Oscillation (NAO), the Atlantic Meridional Overturning Circulation (AMOC), the Mediterranean Overflow Water (MOW) and the subpolar gyre (SPG). The contractions and expansions of the SPG apparently play a key role. This was particularly obvious in the mid-1990s, when the SPG abruptly contracted with the result that warm subtropical water masses moved to the north and east. Small pelagic fish populations in the eastern North and Central Atlantic, including those in the Mediterranean responded quickly by changing abundances and migrating northwards. It seems that the complex ocean-atmosphere changes in the mid-1990s, which are described in the text in detail, caused a regime shift in the ecosystems of the eastern North and Central Atlantic and the small pelagic clupeoid fish populations are the sentinels of this shift.
机译:北部北部和东部大西洋中的小上层类蝶形鱼类的丰度和迁移动态,例如an鱼(Engraulis encrasicolus),沙丁鱼(Sardina pilchardus),沙丁鱼(Sardinella aurita),鲱鱼(Sprattus sprattus)和鲱鱼(Clupea harengus)塞内加尔和挪威之间的变化与大西洋多年代际涛动(AMO)的温暖和寒冷阶段同步变化。通过收集有关渔获量和轶事观察的回顾性数据可以证明这一点,在某些情况下可以追溯到19世纪中叶。 AMO被定义为北大西洋(北纬0-60度)海面温度异常的趋势下降平均值。但是,温度并不是驱动小中上层鱼类种群动态的主要因素。相反,AMO似乎是北大西洋大气-海洋耦合系统中复杂过程的代理。这表现为当前系统的强度和方向发生了大规模变化,使水团在北大西洋附近移动,并可能涉及北大西洋涛动(NAO),大西洋子午翻转环流(AMOC),地中海溢流水(MOW) )和亚极回旋(SPG)。 SPG的收缩和膨胀显然起着关键作用。这在1990年代中期特别明显,当时SPG突然收缩,结果亚热带暖水团块向北和向东移动。北部东部和中大西洋的小型中上层鱼类种群(包括地中海鱼类)迅速改变了种群数量并向北迁移,从而做出了迅速反应。似乎在1990年代中期发生了复杂的海洋-大气变化,这在文本中有详细描述,这导致了北部北部和中部大西洋的生态系统发生了政权转移,而小型中上层类鳞茎鱼类种群就是这种情况的定点。转移。

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