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Interannual variability of alongshore spring bloom dynamics in acoastal sea caused by the differential influence of hydrodynamicsand light climate

机译:水动力和轻气候的差异影响引起的沿海近岸春季水华动态的年际变化

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Timing and spatial distribution of phytoplanktonblooms in coastal oceans are highly variable. The interac-tions of various biological and physical factors leading to theobserved variability are complex and remain poorly under-stood. We present an example for distinct differences in thespatio-temporal chlorophyll a (CHL-a ) distribution on aninterannual scale, integrating high-frequency data from anautonomous measuring device (FerryBox), which operatedon an alongshore route in the coastal German Bight (NorthSea). While in one year the distribution of CHL-a was spa-tially homogeneous (2004), a bloom only developed in onepart of the transect in the following spring period (2005). Weuse a one-dimensional Lagrangian particle tracking model,which operates along the mean current direction, combinedwith a NPZ-model to identify the mechanisms controllingthe observed interannual bloom variability on the alongshoretransect. Our results clearly indicate that in 2004 the locallight climate determined the spatial and temporal dynam-ics of the spring bloom. In contrast, the import of a watermass with elevated CHL-a concentrations from the adjacentSouthern Bight triggered the spring bloom in 2005. The in-flow event did, however, not last long enough to spread thebloom into the eastern part of the study area, where highturbidity prevented local phytoplankton growth. The modelidentifies two interacting mechanisms, light climate and hy-drodynamics, that controlled the alongshore dynamics. Es-pecially the occurrence of a pronounced spring bloom despiteunfavourable light conditions in 2005 underlines the need tocarefully consider hydrodynamics to understand the dynam-ics of the plankton community in coastal environments.
机译:沿海海洋浮游植物开花的时间和空间分布是高度可变的。导致观察到的变异性的各种生物学和物理因素之间的相互作用是复杂的,并且仍然难以理解。我们提供了一个示例,说明了在年度尺度上时空叶绿素a(CHL-a)分布的明显差异,该示例整合了来自自动测量设备(FerryBox)的高频数据,该设备在德国沿海(NorthSea)的沿海路线上运行。尽管一年之内CHL-a的分布在空间上是均匀的(2004年),但在随后的春季(2005年),仅在该样条的一部分中出现了水华。我们使用沿平均电流方向运行的一维拉格朗日粒子跟踪模型,并结合NPZ模型,以识别控制沿岸样带观测到的年华变化的机制。我们的结果清楚地表明,在2004年,局部光照气候决定了春暖花开的时空动力。相比之下,从邻近的南海岸线进口的CHL-a浓度较高的水质引发了2005年的春季开花。然而,流入事件的持续时间不足以将花药扩散到研究区域的东部,高浊度阻止了局部浮游植物生长的地方。该模型确定了两种相互作用的机制,即轻度气候和水动力,控制着沿海动力学。尤其是在2005年尽管光线条件不利的情况下仍出现明显的春季开花,这突出表明需要仔细考虑流体力学以了解沿海环境中浮游生物群落的动力学。

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