Weather and climate induced spatial variability of surface suspended particulate matter concentration in the North Sea and the English Channel

Michael Fettweis , Jaak Monbaliu , Matthias Baeye , Bouchra Nechad , Dries Van den Eynde
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引用次数: 37

Abstract

Images from the Moderate Resolution Imaging Spectroradiometer (MODIS) satellite have been used to investigate the meteorological and climate induced variability of suspended particulate matter (SPM) concentration in the North Sea. The meteorology has been characterized by the 11 weather types deduced from a refined system of Lamb’s classification of synoptic weather charts. Climatological effects have been related to the North Atlantic Oscillation index. The surface SPM concentration maps from MODIS have been ensemble averaged according to these weather types or climatological conditions. The data show that each type has a distinct distribution of surface SPM concentration in the North Sea. The differences are explained by different hydrodynamic and wave conditions. The occurrence of storms will impact the shallow regions by increasing the resuspension of bottom material. Prevailing winds will, on the other hand, change the residual transport of SPM in the North Sea. The more protected Southern Bight exhibits relatively stronger influences of advection, whereas in the central North Sea and the German Bight resuspension is more pronounced. This patterns result in an alternation of relatively high SPM concentration in the Southern Bight and in the rest of the southern North Sea during certain weather conditions. Limitations in satellite images have been assigned to stratification effects due to the occurrence of highly concentrated mud suspensions during certain weather types. The approach provides a tool to improve our understanding of coastal and shelf sea processes, especially with respect to variations of SPM concentration distribution according to weather, climate and climate change.

天气和气候诱导北海和英吉利海峡海面悬浮颗粒物浓度的空间变异
利用中分辨率成像光谱仪(MODIS)卫星的图像,研究了北海悬浮颗粒物(SPM)浓度的气象和气候变化。从兰姆天气天气图分类的精细化系统中推断出了11种天气类型。气候效应与北大西洋涛动指数有关。根据这些天气类型或气候条件对MODIS的地表SPM浓度图进行了总体平均。数据表明,每种类型的海面SPM浓度在北海有明显的分布。不同的水动力和波浪条件解释了这种差异。风暴的发生将通过增加底部物质的再悬浮来影响浅层地区。另一方面,盛行风将改变北海SPM的残余输送。受保护程度较高的南湾受平流影响相对较强,而北海中部和德国湾受平流影响较明显。这种模式导致在某些天气条件下,南湾和北海南部其他地区的SPM浓度相对较高。由于在某些天气类型下会出现高度集中的泥浆悬浮物,因此卫星图像的分层效应受到限制。该方法提供了一个工具,以提高我们对沿海和陆架海过程的理解,特别是关于SPM浓度分布随天气、气候和气候变化的变化。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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