The impact of LNG offshore terminal on sea temperature and sea currents in the northern Adriatic Sea

IF 2.3 3区 环境科学与生态学 Q1 MARINE & FRESHWATER BIOLOGY
Gorana Jelić Mrc̓elić, Majda Jurić, N. Supić, MaMATHIEU thieu DUTOUR SIKIRIĆ
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引用次数: 0

Abstract

The aim of this paper is to simulate the impact of a potential offshore LNG terminal on sea temperature (in autumn and spring/ summer) and sea currents (in autumn/winter) at three different depths (at the sea surface, at 25 m depth and at the seabed) in the northern Adriatic Sea from 14 November 2015 to 06 August 2016 using the Regional Ocean Modelling System (ROMS) model. The location of the potential offshore LNG terminal Istria (in the northern Adriatic Sea) was selected using the visual PROMETHEE method. The potential LNG terminal uses seawater for LNG heating and the seawater cooled to a temperature of 9°C returns to the marine environment. Although the differences in sea temperature with and without the discharge fit within normal temperature ranges, the simulations show that the discharge changed the speed and direction of sea currents at the sea surface not only in the wider northern Adriatic, but in the entire Adriatic. This is probably due to the specific circulation in the Adriatic, where cold water affects the geostrophic balance, an important part of the circulation field that depends on density (a function of salinity and temperature). Atmospheric conditions in the broader vicinity of the LNG terminal would also be affected by redistribution of air-sea fluxes due to changes in surface temperature. Changes in circulation would alter environmental conditions by redistributing nutrients, oxygen, etc. Further multi-year simulations of changes in the circulation system are needed, but other physical parameters (density, salinity, river inflow...) should also be included in the simulations to determine the cumulative impact of a potential LNG terminal on the marine environment.
LNG海上接收站对亚得里亚海北部海温和海流的影响
本文的目的是使用区域海洋建模系统(ROMS)模型,模拟2015年11月14日至2016年8月6日期间,潜在的海上液化天然气接收站对亚得里亚海北部三个不同深度(海面、25米深度和海床)的海水温度(秋季和春季/夏季)和洋流(秋季/冬季)的影响。使用可视化PROMETHEE方法选择了潜在的海上液化天然气接收站Istria(位于亚得里亚海北部)的位置。潜在的液化天然气接收站使用海水进行液化天然气加热,冷却至9°C的海水返回海洋环境。尽管有流量和没有流量的海水温度差异都在正常温度范围内,但模拟表明,流量不仅改变了整个亚得里亚海更广阔的北部海面的洋流速度和方向。这可能是由于亚得里亚海的特定环流,那里的冷水影响地转平衡,地转平衡是环流场的重要组成部分,取决于密度(盐度和温度的函数)。液化天然气接收站附近的大气条件也会受到地表温度变化引起的海气通量再分配的影响。循环的变化会通过重新分配营养物质、氧气等来改变环境条件。需要对循环系统的变化进行进一步的多年模拟,但模拟中还应包括其他物理参数(密度、盐度、河流流入量…),以确定潜在液化天然气接收站对海洋环境的累积影响。
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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来源期刊
Mediterranean Marine Science
Mediterranean Marine Science MARINE & FRESHWATER BIOLOGY-
CiteScore
5.20
自引率
17.90%
发文量
34
审稿时长
>12 weeks
期刊介绍: The journal Mediterranean Marine Science (MMS), published by the Hellenic Centre for Marine Research (HCMR), issues three volumes annually. The journal welcomes original research articles, short communications, New Mediterranean Biodiversity records, extended reviews, comments, and Theme sections in all fields of Oceanography, Marine Biology, Marine Conservation, Fisheries and Aquaculture in the Mediterranean area and the adjacent regions. All content is peer reviewed.
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