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Numerical modelling of physical processes governing larval transport in the southern North Sea

机译:北海南部控制幼体运输的物理过程的数值模拟

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A three-dimensional hydrodynamic model (GETM) was coupled with a particle tracking routine (GITM) to study the inter-annual variability in transport paths of particles in the North Sea and English Channel. For validation, a comparison with observed drifter trajectories is also presented here. This research investigated to what extent variability in the hydrodynamic conditions alone (reflecting passive particle transport) contributed to inter-annual variability in the transport of eggs and larvae. In this idealised study, no a priori selection of specific spawning grounds or periods was made and no active behaviour (vertical migration) or mortality was included. In this study, egg and larval development towards coastal nursery areas was based solely on sea water temperature, while settlement areas were defined by a threshold water depth. Results showed strong inter-annual variability in drift direction and distance, caused by a combination of wind speed and direction. Strong inter-annual variability was observed both in absolute amount of settlement in several coastal areas, and in the relative importance of the different areas. The effects of wind and temperature variability are minor for settlement along the western shores of the North Sea and in the English Channel, but have a very significant impact on settlement along the eastern shores of the North Sea. Years with strong south-westerly winds across the Dover Straight resulted in higher settlement figures along its eastern shores of the North Sea (standard deviation 37% of the mean annual settlement value). Settlement in the western Dutch Wadden Sea did not only show inter-annual variability, but patterns were also variable within each year and revealed seasonal changes in the origin of particles: during winter, stronger currents along with colder temperatures generally result in particles originating from further away.
机译:将三维流体动力学模型(GETM)与粒子跟踪例程(GITM)耦合,以研究北海和英吉利海峡中粒子传输路径的年际变化。为了验证,此处还提供了与观察到的漂移轨迹的比较。这项研究调查了仅在流体动力学条件下的可变性(反映了被动粒子的运输)在多大程度上有助于卵和幼虫的运输的年际变化。在这项理想的研究中,没有事先选择特定的产卵场或产卵期,也没有包括活跃行为(垂直迁移)或死亡率。在这项研究中,卵和幼体向沿海苗圃地区的发育完全基于海水温度,而定居区域则由阈水深来定义。结果表明,由于风速和风向的结合,漂移方向和距离的年际变化很大。在几个沿海地区的绝对沉降量以及不同地区的相对重要性中均观察到强烈的年际变化。对于北海西岸和英吉利海峡的沉降,风和温度变化的影响较小,但对北海东岸的沉降影响很大。多佛河道西南偏南风的年份,导致其北海东岸的沉降数字更高(标准偏差为年平均沉降值的37%)。荷兰西部瓦登海的沉降不仅显示出年际变化,而且模式每年都在变化,并且揭示出颗粒物起源的季节性变化:在冬季,较强的水流和较低的温度通常导致颗粒物从更深处起源。远。

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