全天候海冰气象监测系统可靠性研究

目的】为了减少海冰对平台生产所造成的影响,JZ9-3海域首次引用了全天候海冰气象监测系统。为了确保系统的正常运行,需要对系统进行可靠性评估。【方法】采用动态模糊故障树法,对全天候海冰气象监测系统的可靠性进行评估,同时提出初步的预防措施。【结果】通过应用动态模糊故障树对系统可靠性进行评估,获取了系统的薄弱环节,并提出了有效措施对薄弱环节加以控制。【结论】通过研究,有效地提高了系统的可靠性,这也是动态模糊故障树在国内的首次应用,为未来动态模糊故障树的广泛应用奠定基础。     

利用伪速度方法压制浅海鬼波

采用基于用传统方法获取的海上单分量地震资料, 估算出同一位置速度的垂直分量(伪速度), 再与单分量压力数据联合, 达到压制鬼波的目的。将稀疏约束的反卷积方法作为鬼波压制的关键环节, 使得在浅海环境下, 由海水表面引起的检波器端上、下行波干涉产生的陷波问题得到改善, 同时低频能量得到增强, 提高了数据的分辨率。该方法可用于海上单分量压力数据的再处理, 拓宽数据的频带范围。     

海堤渗压神经网络分布模型的建立及规律分析

为有效揭示海堤渗压的分布特征,掌握其在临海工作环境下的特殊规律,在利用神经网络建模优点的同时,采用多测点渗压监控信息,并将测点坐标因素加入到输入层,综合前期潮位因子、积分型降雨因子、时效因子,形成海堤渗压神经网络安全监控分布模型结构,以实测信息进行建模训练计算;在获得合理训练结果基础上,根据输入层因子补充插入坐标样本,获得不同位置的渗压模型值及渗压分布曲线.文中以广义回归神经网络为例,结合浦东海堤实测资料,以实例说明以上述方法在神经网络不提供显式的情况下,建立可获得分布曲线的监控模型,并以此对海堤渗压分布规律特色加以分析.     

南大西洋至几内亚湾冬季海浪传播特性

为解决南大西洋至几内亚湾海域的海浪组成成分、传播特性及来源这3个该海域一直需要解决的问题，建立SWAN （Simulating WAves Nearshore）双层嵌套海浪模型对南大西洋至几内亚湾冬季海浪时空分布进行模拟分析，结果表明：南大西洋海浪有效波高呈高纬度区（30°S以南）向低纬度区（30°S以北）递减的趋势 ，高纬度区海浪传播方向与风场关系密切，低纬度区则与风场差异明显；南大西洋涌浪波高与混合浪波高分布高度相关，涌浪在混合浪中所占比例较大，尤其在风速较小的低纬度海域更为显著；南大西洋中部至几内亚湾存在相对固定的S-SW涌浪系统，其能量在二维海浪谱上分布集中，空间方向上分布范围较窄；模拟时段内几内亚湾呈明显的涌浪主导状态，通过对有效波高最大时刻的一次涌浪过程溯源发现，影响几内亚湾的涌浪可追溯至约6.5天前南大西洋咆哮西风带海域的强风浪。     

特殊地理形态下的胶东传统民居——以烟台养马岛古村落为例

民居的形成和发展受到很多因素的制约,如自然因素、社会文化因素、经济因素和技术因素等.其中对于一些特殊地理形态下的民居,自然因素的影响就更为明显,以烟台养马岛为例,通过对胶东传统民居在山、海、岛的特殊地理形态下所形成的独具一格的建筑形态的描述,从"山地"、"滨海"、"岛居"3个方面分析自然环境对于民居形成与发展的重要影响...     

Simulation of sea surface temperature changes in the Middle Pliocene warm period and comparison with reconstructions

The Middle Pliocene (ca 3.12–2.97 Ma) is a recent warm period in the Earth’s history. In many respects, the warmth of the Middle Pliocene is similar to the probable warm situation of the late 21st century predicted by climate models. Understanding the Middle Pliocene climate is important in predicting the future climate with global warming. Here, we used the latest reconstructions for the Middle Pliocene—Pliocene Research Interpretation and Synoptic Mapping (PRISM) version 3—to simulate the Middle Pliocene ...     

Sea surface temperature records of core ZY2 from the central mud area in the South Yellow Sea during last 6200 years and related effect of the Yellow Sea Warm Current

Sea surface temperature (SST) records in the South Yellow Sea during the last 6200 years are reconstructed by the unsaturation index of long-chain alkenones (K 37 U ’) in sediment core ZY2 from the central mud area.The SST records varied between 14.1 and 16.5°C (15.6°C on average),with 3 phases:(1) A high SST phase at 6.2-5.9 cal ka BP;(2) A low and intensely fluctuating SST phase at 5.9-2.3 cal ka BP;and (3) A high and stable SST phase since 2.3 cal ka BP.Variation of the SST records is similar to intensity of the Kuroshio Current (KC),and corresponds well in time to global cold climate events.However,the amplitude of the SST response to cooling events was significantly different in different phases.The SST response to global cooling event was weak while the KC was strong;and the SST response was strong while the KC was weak.The difference in amplitude of the SST response is possibly caused by the modulation effect of the Yellow Sea Warm Current which acts as a shelf branch of the KC and a compensating current induced by the East Asia winter monsoon.The warm waters brought by the Yellow Sea Warm Current cushion the SST decrease induced by climate cooling,and both the Kuroshio and East Asian winter monsoon play important roles in the modulation mechanism.The SST records display a periodicity of 1482 years.The same period was found in the KC records,indicating that variation of the SST records in the central South Yellow Sea is strongly affected by KC intensity.The same period was also found in Greenland ice cores and North Atlantic and Arabian Sea sediment cores,showing a regional response of marine environmental variability in the East China Seas to that in the global oceans.     

工业废渣对海泥烧结砖泛霜程度影响的试验

研究两种不同特性工业废渣铁尾矿、粉煤灰对海泥烧结多孔砖样品泛霜程度的影响及机理.结果表明:铁尾矿减轻海泥烧结砖泛霜程度的有利因素多,粉煤灰提高海泥烧结砖泛霜程度的不利因素多.此外,掺加外加剂可以在某种程度上降低海泥烧结砖的泛霜等级;当掺量达到某一范围时,能够较大幅度减少砖坯成型用水量,烧成中产生液相的非瘠性工业废渣-铁...     

Sea surface temperature east of Australia： A predictor of tropical cyclone frequency over the western North Pacific？

The relationship between sea surface temperature (SST) east of Australia and tropical cyclone frequency over the western North Pacific (WNPTCF) is analyzed by use of observation data.The WNPTCF from June to October is correlated negatively to spring SST east of Australia.When the spring SST is in the positive phase,a cyclonic circulation anomaly in the upper troposphere and an anticyclonic circulation anomaly in the lower troposphere prevail over the western North Pacific from June to October,concurrent with an anomalous atmospheric subsidence and an enlarged vertical zonal wind shear.These conditions are unfavorable for tropical cyclone genesis,and thus WNPTCF decreases.The negative phase of the spring SST east of Australia leads to more tropical cyclones over the western North Pacific.The spring SST east of Australia may give rise to simultaneous change in tropical atmospheric circulation via the teleconnection wave train,and then subsequently affect atmospheric circulation variation over the western North Pacific.     

海上要地防空反导阵地优度排序研究

针对海上要地防空反导作战中发射阵地优度排序问题,结合要地面积较小、各备选阵地自然环境条件差别不大的实际情况,提出一种以各阵地与保卫目标间距离来衡量阵地优度的评价指标体系构建方法。首次将各己方目标的重要度作为对应评价指标的权值,并提出一种基于网页排名(PageRank, PR)算法的评价指标赋权方法。通过算例仿真可得,本文提出的方法能够给出科学、准确的备选阵地优度排序,为解决海上要地防空反导阵地选择问题提供了一种新思路、新方法。