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Coastal Environment, Disaster, and Infrastructure - A Case Study of China's Coastline最新文献

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Long-Term Sea Level Variability in the Yellow Sea and East China Sea 黄海和东海海平面的长期变化
Ying Xu, Mingsen Lin, Q. Zheng
Using the satellite altimeter maps of sea level anomaly (MSLA) and tidal gauge data, this chapter gives an investigation of the long-term sea level variability (SLV) and sea level rise (SLR) rate in the Yellow Sea (YS) and East China Sea (ECS). Correlation analysis shows that the satellite altimeter is effective and capable of revealing the coastal SLV. To investigate the regional correlation of SLV in the YS and ECS, tidal gauge station data are used as references. Based on the monthly maps of correlation coefficient (CC) of SLV at tidal stations with the gridded MSLA data, we find that the existence of Kuroshio decreases the correlation between the coastal and Pacific sea levels. The empirical mode decomposition (EMD) method is applied to derive the SLR trend on each MSLA grid point in the YS and ECS. According to the two-dimensional geographical distribution of the SLR rate, one can see that the sea level on the eastern side of the Kuroshio mainstream rises faster than that on the western side. Both the YS and ECS SLR rates averaged over 1993–2010 are slower than the globally averaged SLR rate. This implies that although the SLV in the two seas is affected by global climate change, it could be mostly influenced by local effects.
利用卫星高度计海平面异常图(MSLA)和测潮资料,对黄海(YS)和东海(ECS)的长期海平面变率(SLV)和海平面上升率(SLR)进行了研究。相关分析表明,卫星高度计是有效的,能够显示沿海SLV。为了研究YS和ECS中SLV的区域相关性,以潮站资料为参考。利用栅格化的MSLA数据对潮汐站SLV相关系数(CC)逐月图进行分析,发现黑潮的存在降低了沿海与太平洋海平面的相关性。应用经验模态分解(EMD)方法推导了YS和ECS中每个MSLA网格点上的SLR趋势。从单反率的二维地理分布可以看出,黑潮主流东侧海平面上升速度快于西侧海平面上升速度。1993-2010年美国和欧洲的平均单反利率都低于全球平均单反利率。这表明,尽管两海的SLV受到全球气候变化的影响,但它可能主要受到局部效应的影响。
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引用次数: 0
Coastal Upwelling Off the China Coasts 中国沿海上升流
Jianyu Hu, X. Liang, Hongyang Lin
Upwelling is an important oceanographic phenomenon that brings cooler and nutrient- rich water upward to the surface, facilitating the growth of phytoplankton and other primary producers, which results in high levels of primary productivity and hence fish - ery production. This chapter presents a review of recent studies on six major upwelling regions along the China coasts, with a focus on the eastern and southeastern coasts of mainland China, based on in situ measurements, satellite observations and numerical simulations. These upwelling regions result primarily from the summer monsoon winds, though other mechanisms, such as river discharge, baroclinicity, topography, tides, and the presence of mean current, may also be in play. In this review, their impacts on local biogeochemical processes are briefly summarized. Also discussed are their possible responses to the globally changing climate.
上升流是一种重要的海洋学现象,它将较冷和富含营养的水带到海面,促进浮游植物和其他初级生物的生长,从而产生高水平的初级生产力,从而提高鱼类产量。本章综述了中国沿海6个主要上升流区域的最新研究进展,重点介绍了中国大陆东部和东南部沿海地区的现场测量、卫星观测和数值模拟。这些上升流区域主要是由夏季季风造成的,尽管其他机制,如河流流量、斜压性、地形、潮汐和平均洋流的存在也可能起作用。本文就其对当地生物地球化学过程的影响作一综述。还讨论了它们对全球气候变化的可能反应。
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引用次数: 3
Analysis for the Effect of Sea Surface Temperature (SST) on the Coastal Environments of Jiangsu Province, China 海面温度对江苏省沿海环境的影响分析
Chenxu Ji, Yuanzhi Zhang, Kapo Wong, Yu Li, Ting-chen Jiang, Liang Xiangsan, Xia Lu
In this chapter, we present the analysis for the effect of summertime SST on the coastal environments of Jiangsu province, China. We analyze the relationship between the SST and the Jiangsu precipitation in summer based on GPCP’s precipitation data and NOAA’s SST data from 1979 to 2011, using approaches that include correlation analysis, regression analysis, and lead-lag analysis. The results show that certain strong oceanic signals affect summer Jiangsu precipitation, showing that SST of some oceanic areas significantly affect the precipitation of Jiangsu in summer. By the lead-lag analysis, it is found that the spring SST plays an important role in the summer precipitation in the coastal areas of Jiangsu, China.
在这一章中,我们分析了夏季海温对中国江苏省沿海环境的影响。利用1979 ~ 2011年GPCP降水资料和NOAA海温资料,采用相关分析、回归分析和超前-滞后分析等方法,对江苏夏季海温与降水的关系进行了分析。结果表明,某些强海洋信号影响江苏夏季降水,表明部分海域海温对江苏夏季降水有显著影响。通过超前滞后分析,发现春季海温对江苏沿海地区夏季降水具有重要影响。
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引用次数: 0
Nuclear Pollution in the East China Sea from the Fukushima Disaster 福岛核事故对东海的核污染
X. Liang, Yineng Rong
Nuclear pollution has become a new form and perhaps more harmful type of pollution that obsesses coastal regions; it has been of increasing concern after the disastrous Fukushima nuclear leak on March 11, 2011. In order to assess the impact of the Fukushima accident on the East China Sea (ECS), a highly resolved model is set up to simulate the evolution of the Cs concentration. Different from previous studies in this regard, here we take into account the radionuclides originally existing in the ocean. It is found that the radionuclides from the Fukushima leak do have reached ECS, though with a concentration far below the harmful level. The major waterways that inlet the radionuclides are Taiwan Strait and the waterway east of Taiwan. The radioactive material tends to accumulate in the ECS until reaching its peak in 2019; afterward, the outflux through Tokara Strait and Tsushima exceeds the influx through the two southern waterways, and the material resumes in 2021 to its original state. The concentration is neither homogeneously nor stationarily distributed; for example, usually in summer, there is a high center over the Subei Bank in the Yellow Sea. This study is expected, should a similar accident happen again, to help decide where to monitor the ocean, and, hopefully, how to get the pollution under control.
核污染已成为困扰沿海地区的一种新形式、或许危害更大的污染;在2011年3月11日灾难性的福岛核泄漏事件之后,这一问题日益引起人们的关注。为了评估福岛核事故对东海的影响,建立了一个高分辨率模型来模拟Cs浓度的演变。与以往在这方面的研究不同,这里我们考虑了原来存在于海洋中的放射性核素。发现福岛泄漏的放射性核素确实达到了ECS,尽管浓度远低于有害水平。放射性核素流入的主要水道是台湾海峡和台湾以东的水道。放射性物质倾向于在ECS中积累,直到2019年达到峰值;之后,通过托卡拉海峡和对马岛的流出量超过了通过南部两条水道的流入量,材料在2021年恢复到原来的状态。浓度分布既不均匀也不平稳;例如,通常在夏天,在黄海苏北岸上有一个高中心。如果类似的事故再次发生,这项研究有望帮助决定在哪里监测海洋,以及如何控制污染。
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引用次数: 0
The Slow Coastal-Trapped Waves off Subei Bank in the Yellow Sea and Their Climatic Change in the Past Decades 黄海苏北滩慢阻波及其近几十年的气候变化
X. Liang
Coastal-trappedwaves (CTWs) areaclassofsubinertial signalsin theweatherfrequencyband that playa pivotal role in coastal air-sea interaction. However, this important topic seems to be missingintheheateddebateinrecentyearsoncoastalenvironmentalchangeandprotection.In thischapter,abriefbutself-containedintroductionoftheCTWtheoryispresented,inthehopeofprovidingareferenceforinvestigatorsintherelevantfields.Alsopresentedisanumerical scheme for computing the wave properties. As a demonstration, we have conducted a prelim-inarystudyoftheCTWsforasectionacrosstheSubeiBankintheYellowSea.Bytheresults,allthecomputedslowmodes,includingabottom-intensifiedone,seemtobeslowingdownsince two decades ago. They have particularly slowed down in the event when a strong El Niño is followedbyastrongLaNiña,suchasinthe97 – 98and09 – 10ElNiñoevents.
海岸捕获波(CTWs)是天气频带中的一类亚惯性信号,在沿海海气相互作用中起着关键作用。然而,这个重要的话题似乎在最近几年关于沿海环境变化和保护的激烈辩论中被忽视了。在本章,abriefbutself-containedintroductionoftheCTWtheoryispresented inthehopeofprovidingareferenceforinvestigatorsintherelevantfields。给出了计算波浪特性的数值格式。为了证明这一点,我们已经对黄海苏北岸的河段进行了初步的研究。因此,自20年前以来,所有计算出的慢模态,包括底部强化模态,似乎都在下降。当强厄尔尼诺现象Niño为followedbyastrongLaNiña时,比如97 - 98和09 - 10ElNiñoevents,它们的速度会特别慢。
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引用次数: 0
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Coastal Environment, Disaster, and Infrastructure - A Case Study of China's Coastline
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