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Igor P. Semiletov Irina I. Pipko Irina Repina Natalia E. Shakhova 《Journal of Marine Systems》2007,66(1-4):204
Climatic changes in the Northern Hemisphere have led to remarkable environmental changes in the Arctic Ocean, which is surrounded by permafrost. These changes include significant shrinking of sea-ice cover in summer, increased time between sea-ice break-up and freeze-up, and Arctic surface water freshening and warming associated with melting sea-ice, thawing permafrost, and increased runoff. These changes are commonly attributed to the greenhouse effect resulting from increased atmospheric carbon dioxide (CO2) concentration and other non-CO2 radiatively active gases (methane, nitrous oxide). The greenhouse effect should be most pronounced in the Arctic where the largest air CO2 concentrations and winter–summer variations in the world for a clean background environment were detected. However, the air–land–shelf interaction in the Arctic has a substantial impact on the composition of the overlying atmosphere; as the permafrost thaws, a significant amount of old terrestrial carbon becomes available for biogeochemical cycling and oxidation to CO2. The Arctic Ocean's role in determining regional CO2 balance has been ignored, because of its small size (only 4% of the world ocean area) and because its continuous sea-ice cover is considered to impede gaseous exchange with the atmosphere so efficiently that no global climate models include CO2 exchange over sea-ice. In this paper we show that: (1) the Arctic shelf seas (the Laptev and East-Siberian seas) may become a strong source of atmospheric CO2 because of oxidation of bio-available eroded terrestrial carbon and river transport; (2) the Chukchi Sea shelf exhibits the strong uptake of atmospheric CO2; (3) the sea-ice melt ponds and open brine channels form an important spring/summer air CO2 sink that also must be included in any Arctic regional CO2 budget. Both the direction and amount of CO2 transfer between air and sea during open water season may be different from transfer during freezing and thawing, or during winter when CO2 accumulates beneath Arctic sea-ice; (4) direct measurements beneath the sea ice gave two initial results. First, a drastic pCO2 decrease from 410 μatm to 288 μatm, which was recorded in February–March beneath the fast ice near Barrow using the SAMI-CO2 sensor, may reflect increased photosynthetic activity beneath sea-ice just after polar sunrise. Second, new measurements made in summer 2005 beneath the sea ice in the Central Basin show relatively high values of pCO2 ranging between 425 μatm and 475 μatm, values, which are larger than the mean atmospheric value in the Arctic in summertime. The sources of those high values are supposed to be: high rates of bacterial respiration, import of the Upper Halocline Water (UHW) from the Chukchi Sea (CS) where values of pCO2 range between 400 and 600 μatm, a contribution from the Lena river plume, or any combination of these sources. 相似文献
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基于可靠度理论,进行了允许越浪条件下海堤越浪量的可靠度分析,建立了允许越浪条件下海堤越浪量的极限状态方程。以青岛某斜坡式海堤为例,将有效波高和谱峰周期作为基本随机变量进行越浪量可靠度分析。首先对有效波高和谱峰周期进行Log-normal、Gumbel分布拟合,根据拟合结果,二者均采用Log-normal分布,然后采用Monte Carlo模拟计算了该海堤越浪量的可靠性指标。计算结果表明:进行允许越浪条件下海堤越浪量的可靠度分析是可行的,并且海堤越浪量的可靠性指标概率意义明确,比允许越浪量标准更合理。 相似文献
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本文主要研究在非线性混合海况(即风浪和涌浪组合海况)下,以NREL 5MW_Baseline Monopile近海风机为研究对象,对其塔筒底部(基线)所受到的剪力和弯矩载荷的动力响应进行仿真。在近海风机的时域仿真中,选用了Ochi-Hubble六参数波浪谱,并编制了该谱的程序嵌入到FAST中进行编译。计算过程中,共进行了20次10 min的仿真分析。对于得到的短期载荷,给出了波高程,塔筒底部首尾向剪力和弯矩在线性与非线性不规则波作用下的时程曲线对比图。采用分块最大值法对每一次的短期载荷提取极值,并基于20次仿真所得的极值,给出了塔筒底部首尾向剪力与弯矩在线性与非线性不规则波作用下的超越概率曲线对比图。研究表明,在非线性混合海况下进行近海风机塔筒底部载荷的动力响应研究,计算结果对工程实际应用具有指导意义。 相似文献
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熊雷 《武汉理工大学学报(交通科学与工程版)》2007,31(6):1125-1127,1131
强海浪中小目标回波的检测一直是船用雷达目标识别的难点,但现有的统计方法难以准确和全面地描述复杂的海杂波特性.要突破这一局限性,以获得对复杂现象更有效的描述,就迫切要求使用新技术.文中利用小波理论,针对强海浪下点目标和低矮宽大目标二类以往难以检测的目标,通过区分噪声、点目标、低矮宽大目标在小波变换下不同的奇异特征、设计了一套能够识别出点目标和低矮宽大目标的方案. 相似文献