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A synthetic map of the north-west European Shelf sedimentary environment for applications in marine science

机译:西北欧洲大陆架沉积环境的综合图,用于海洋科学

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Seabed sediment mapping is important for a wide range of marine policy, planning and scientific issues, and there has been considerable national and international investment around the world in the collation and synthesis of sediment datasets. However, in Europe at least, much of this effort has been directed towards seabed classification and mapping of discrete habitats. Scientific users often have to resort to reverse engineering these classifications to recover continuous variables, such as mud content and median grain size, that are required for many ecological and biophysical studies. Here we present a new set of 0.125° by 0.125° resolution synthetic maps of continuous properties of the north-west European sedimentary environment, extending from the Bay of Biscay to the northern limits of the North Sea and the Faroe Islands. The maps are a blend of gridded survey data, statistically modelled values based on distributions of bed shear stress due to tidal currents and waves, and bathymetric properties. Recent work has shown that statistical models can predict sediment composition in British waters and the North Sea with high accuracy, and here we extend this to the entire shelf and to the mapping of other key seabed parameters. The maps include percentage compositions of mud, sand and gravel; porosity and permeability; median grain size of the whole sediment and of the sand and the gravel fractions; carbon and nitrogen content of sediments; percentage of seabed area covered by rock; mean and maximum depth-averaged tidal velocity and wave orbital velocity at the seabed; and mean monthly natural disturbance rates. A number of applications for these maps exist, including species distribution modelling and the more accurate representation of sea-floor biogeochemistry in ecosystem models. The data products are available from https://doi.org/10.15129/1e27b806-1eae-494d-83b5-a5f4792c46fc.
机译:海底沉积物测绘对于广泛的海洋政策,规划和科学问题非常重要,并且在沉积物数据集的整理和综合方面,世界各地都有大量的国家和国际投资。但是,至少在欧洲,许多努力都针对海床分类和离散生境的制图。科学用户经常不得不对这些分类进行逆向工程,以恢复许多生态和生物物理研究所需的连续变量,例如泥浆含量和中值粒径。在这里,我们提供了一组新的0.125°x 0.125°分辨率的合成地图,这些合成地图是从比斯开湾到北海和法罗群岛的北部边界的西北欧洲沉积环境的连续特性的。这些地图混合了网格化的调查数据,基于潮汐流和波浪引起的地层剪切应力分布以及测深特性的统计模型值。最近的工作表明,统计模型可以高精度地预测英国水域和北海中的沉积物成分,在这里,我们将其扩展到整个陆架以及其他关键海床参数的制图。这些地图包括泥,沙和砾石的百分比成分;孔隙率和渗透率整个沉积物以及沙子和砾石部分的中值粒径;沉积物中的碳和氮含量;被岩石覆盖的海底面积百分比;海底的平均和最大深度平均潮汐速度和波轨道速度;和平均每月自然干扰率。这些地图有许多应用,包括物种分布模型和生态系统模型中海底生物地球化学的更精确表示。数据产品可从https://doi.org/10.15129/1e27b806-1eae-494d-83b5-a5f4792c46fc获得。

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