沿海地区悬浮颗粒物输送的模拟

A. Pleskachevsky, H. Gunther
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引用次数: 2

摘要

针对北海尺度(水平分辨率为6 nm)开发的三维悬浮颗粒物(SPM)输运模型进行了改进,并应用于北弗里斯兰瓦登海部分区域(水平分辨率为100 m,垂直分辨率为0.5 m)。卫星数据用于分离不同的SPM交换过程,并导出适当的模型参数。该模型计算了三种不同沉降速度的SPM组分在水柱中的分布,以及相应的细泥沙组分在底部上20 cm的分布。由水流和波浪产生的局部剪应力速度控制着沉积、再悬浮和侵蚀过程。在风暴期间,在极浅的水域,波浪在沙洲上产生高达每秒1米的额外电流,在长岸产生约每秒20-40厘米的电流。这对潮汐盆地侵蚀沉积物的输运有重要贡献。因此,通过交互耦合模型系统生成了SPM建模所需的强迫波场和强迫流场。将介绍瓦登海地区SPM模拟的结果,并与独立观测结果进行比较。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Modeling of suspended particulate matter transport in coastal areas
A three-dimensional suspended particulate matter (SPM) transport model, developed for North Sea scales (6 nm horizontal resolution), was improved and applied for a part of the North Frisian Wadden Sea with 100 m horizontal and 0.5 m vertical resolution. Satellite data were used to separate different SPM exchange processes and to derive appropriate model parameters. The model calculates distributions of three SPM fractions with different settling velocities in the water column and of the corresponding fine sediment fractions in the upper 20 cm of the bottom. The local shear stress velocities, derived from currents and waves control the processes of sedimentation, resuspension and erosion. In extreme shallow water during storms, waves generate additional currents up to 1 m/s over sand banks and long-shore currents of about 20-40 cm/s. This is an important contribution to the transport of eroded sediments in tidal basins. Therefore the forcing wave and current fields necessary for SPM modeling were generated by an interactively coupled model system. Results of the SPM simulations in the Wadden Sea area will be presented and compared with independent observations.
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