Wave climate evolution in the Bay of Biscay over two decades

As a background, a review of long term evolution of wave climate in the North Atlantic is discussed. Most studies show that interannual evolutions in wave heights may be related to climatic factors, such as the North Atlantic Oscillation Index for example.Data of a waverider, consisting of a time series of 20 years in the Bay of Biscay (off Biscarosse, France), are analysed. Based on these data obtained from 1980, wave heights tend to decrease over the period. Also, interannual evolutions exist, particularly in the wave period. The fact that the annual wave periods at Biscarosse are found to vary more significantly than the annual wave heights led us to assume that it is an indirect effect of the evolution in the location of generating storms relative to the buoy. The relationships between wave parameters and climatic factors such as the North Atlantic Oscillation Index and the Garonne discharge have been derived: they show that the NAO index is negatively correlated with the river discharge and positively correlated with the wave period. This result is in agreement with the general climate scheme associated with NAO cycle proposed by Kushnir et al. [Kushnir, Y., Cardone, V.J., Cane, M., 1995. Link between Atlantic climate variability of surface wave height and sea level pressure. Proc. Fourth Int. Workshop on Wave Incasting and forecasting, Banff, AB, Canada, 59–64.]: NAO+ shifts storm tracks northward and dry weather are encountered in the southern part of Europe (conversely NAO− brings storm tracks and rainfall closer). Concerning wave heights, the lack of dependence on NAO index may be associated with compensation effects between wind intensity and storm tracks: wave energy is partly dissipated while reaching the Bay of Biscay in case of severe but distant storms (NAO+), which is not the case for storms generated nearer to the buoy and associated with moderate westerly winds (NOA−). However, the reason of the decrease in wave heights is not clear.     

粤港澳大湾区城际铁路网运营管理模式

通过调研分析粤港澳大湾区内城际铁路运营管理现状,分别对城际类、通道类项目的运营管理模式进行分析讨论。对城际类项目,建议可独立运营的线路采用自管自营模式,与国家铁路联通紧密的广珠线可继续委托广州铁路(集团)公司运营,内地与港澳联合运输线路应与相关方签订联合运输协议。对通道类项目,建议按照高速铁路的运营管理选择代管模式。     

The annual cycle of nanoflagellates in the Central Cantabrian Sea (Bay of Biscay)

The annual cycle of nanoflagellates (NF) including autotrophic (ANF), heterotrophic (HNF) and mixotropic (MNF) flagellates carried out in a temperate sea (Central Cantabrian Sea, southern Bay of Biscay) is presented. Three stations with characteristics ranging from coastal to oceanic conditions were analysed in order to compare NF response to this gradient. Samples were monthly collected at each station at three different depths between February 2002 and December 2002. CTD profiles were also taken at each station. NF were grouped according to their trophic status into ANF, HNF and MNF. Abundance and biomass were determined for each group. The annual cycle showed a general pattern consisting in a maximum in July with secondary maxima in March and October and minimum values in May. ANF were the most important fraction, making a major contribution (nearly 75%) to total NF biomass in all stations. HNF represented over 20% along the cycle, except for a peak in spring found in every station. MNF reached less than 5%, showing low seasonability. Small flagellates (2–5 µm) dominated throughout the cycle. Microplankton community was also analysed in terms of abundance and biomass. A significant positive correlation (r² = 0.49) was obtained between 2–5 µm NF and 10–20 µm HNF–MNF biomasses, suggesting a possible trophic relationship between these groups which should be cautiously taken. No significant relationships were found between microplankton and NF or between nutrients and ANF, indicating that the regulation of NF numbers is complex and probably implicates other groups. In addition to this, the unexpected 2002 Chl a concentration pattern and the misplacing of upwelling events render necessary to perform additional studies to fully understand the precise behaviour of NF in the Cantabrian Sea. To the best of our knowledge, this is the first study of a NF cycle in a temperate sea that considers all functional groups.     

关于渤海湾危险货物滚装运输的探讨

文中分析了渤海湾危险货物滚装运输发展的现状，论述了制约危险货物滚装运输的主要因素，提出了相应的改进建议和加强监督管理的措施     

Recent sedimentary study of the shelf of the Basque country

The Northern Iberian margin of the Spanish Basque country (provinces of Gipuzkoa and Viscaia) is characterized by a narrow continental platform, which receives inputs of riverine particulate matter from the numerous riverine systems located within the Basque country. This particulate matter is subsequently deposited within the Bay of Biscay, and Gouf de Capbreton [Frouin, R., Fiuza, A.F.G., Ambar, I., Boyd, T.J., 1990. Observations of a poleward surface current off the coasts of Portugal and Spain during winter. Journal of Geophysical Research 95 (C1), 679–691]. The main goal of this study is to establish a map of the surface sediment distribution of the Basque continental shelf and more specifically to map the muddy patch located at the eastern side of that continental shelf.Three oceanographic cruises were conducted in 2003 and 2004. From these campaigns 340 surface samples, 12 short cores and 3 gravity cores have been collected over the mid and outer shelf from depths ranging between 50 m and 150 m deep. 3 seismic profiles were obtained across the shelf mud patch using a Sparker device.Sediment grain-size analyses were performed by the classical physical method of sieving and use of settling columns. The POC (Particular Organic Carbon) amounts in sediment and water samples were determined using the Strickland and Parsons' method [Strickland, J.D.H., Parsons, T.R., 1972. Determination of particulate carbon. In : A practical handbook of seawater analysis. Fisheries ResearchBoard of Canada, Ottawa, pp. 207−211] as adapted by Etcheber [Etcheber, H., 1981. Comparaison des diverses méthodes d'évaluation des teneurs en matières en suspension et en carbone organique particulaire des eaux marines du plateau continental aquitain. Journal de Recherche Océanographique VI (2), 37−42]. Radioisotopic measurements (²¹⁰Pb_exc) were made using a semi-planar germanium detector coupled to a multichannel analyser. Radiographical analysis was performed with an X-ray equipment (SCOPIX®) coupled with a radioscopy instrumentation and processing unit.Firstly, a detailed sedimentological map of this shelf has been produced and secondly, geophysical surveys have precisely mapped the geometry of the main mud patch on the continental shelf. In the mud patch itself the rates of sedimentation are between 0.13 and 0.50 cm yr^− 1. The maximum rate of sedimentation is located in the central mud patch, whereas the minimum rate of deposition occurs close to the rocky outcrops. These results seem to be in agreement with the estimation of the total thickness of the mud patch revealed by seismic profiles. The central part corresponds to the maximum thickness of 7 m.Interpretations of the associated oceanic current forcing factors (current direction, wave fetch and wind directional modes) relating to the identified sediment depositional zones are also undertaken.     

粤港澳大湾区船舶污染风险分析及防治对策研究

2019年2月18日中共中央、国务院印发了《粤港澳大湾区发展规划纲要》,其中航运清洁发展是重要的内容之一。面对粤港澳大湾区水路运输高速发展的态势,尤其是石油及其制品的运量快速增长,船舶及其有关作业活动对水域环境造成的污染风险越来越大,大湾区内各市均不同程度面临着严峻的船舶污染防治形势。为保障国家、行业以及《规划纲要》关于船舶污染防治措施和要求的落实,本研究对大湾区船舶污染风险进行了分析,梳理了大湾区船舶污染防治现状,并提出了相应的污染防治对策。     

青岛胶州湾海底隧道陆域段近距下穿地表建筑物爆破震动控制技术

青岛胶州湾海底隧道陆域段钻爆施工期间,为确保距隧道拱顶约12 m的地表建筑物安全及隧道大断面掘进,通过采用下导超前、后续大断面扩挖施工方法,运用液压凿岩台车进行大中空孔直眼掏槽及合理化的钻爆设计等技术,将地表建筑物最大垂直震速控制在国标允许范围之内;通过采用孔外中段别雷管接力起爆,实现了大断面（超前下导、后续扩挖面）一次性点火起爆,解决了大断面一次性爆破雷管段别不足的难题;通过爆破震动测试及数据回归分析,得到了震动波在地层中的传播规律,并通过该规律进行药量真正校核。     

杭州湾跨海大桥船舶碰撞风险分析

文中主要对引航锚地海域船桥碰撞风险进行分析,合理识别风险因素,并运用故障树分析法对风险因素进行评估,最后提出风险控制的措施。     

杭州湾北岸深槽潮流动力要素研究

基于杭州湾海域大范围潮流数值模拟的结果,从河口平面边界形态、水下地形、外海潮型等方面,探讨了影响杭州湾北岸深槽的潮流动力要素。发现天然要素以及部分与人类活动相关的要素均对深槽的塑造存在影响。研究成果可为杭州湾北岸深槽的保护和开发提供一定的科学依据。     

福建兴化湾近岸地貌特征与泥沙来源分析

在现场地貌调查及沉积物取样分析的基础上,对兴化湾的自然条件、沉积特征、泥沙来源及运移趋势进行了分析。判明石城岛以西水下沉积物以粘土质粉砂分布为主,泥沙粒径在0.01 mm左右,为河流下泄泥沙沉积为主。石城岛以东局部区域沉积物质为极粗砂,为近岸山体及浅滩冲蚀物质沉积为主。兴化湾的泥沙主要为河流输沙,其次是周边沿岸冲蚀入海物质及岬角岛礁受风浪侵蚀泥沙。由于湾外涨、落潮流路的稳定和潮流动力的强劲,湾内水深地形与潮流动力有很好的对应性和稳定性,泥沙运动仅限于湾内泥沙的再搬运。