Analysis of the Distribution,Rotation and Scale Characteristics of Solar Wind Switchbacks:Comparison between the First and Second Encounters of Parker Solar Probe

The S-shaped magnetic structure in the solar wind formed by the twisting of magnetic field lines is called a switchback,whose main characteristics are the rever...     

一维大气边界层二阶闭合的有限元数值模式 I. 对流边界层模拟

利用有限元法用于二阶湍流闭合大气对流边界层模式,并模拟了Wangara试验33天的对流边界层的发展过程,计算结果表明,该模式能真实的模拟出对流边界层的发展过程,并且准确地反映对流边界层中湍流扩散和输送过程。     

相转移催化合成邻乙氧基苯酚的研究

研究了利用相转移催化反应在不同的条件下合成邻乙氧基苯酚,产率可达７０％以上,并初步探讨了不同类型溶剂对相转移催化反应的影响。     

滇西实验场区地壳密度时变特征与强震机理研究

利用重力与水准资料分析研究了滇西背景单层密度变化图像和1985～1992年单层密度时变特征,结果显示其与断裂活动、地震活动明显相关,特别是1996年丽江地震的孕育可能与洱源至剑川或鹤庆的串珠状低波数时变异常带及背景地壳密度变化梯级带有关。基于此,结合已有地震前兆或孕育模式,从地壳运动角度初步提出了地壳内部密度时变的强震前兆模式或发震机制。     

Anomalously low alkenone temperatures caused by lateral particle and sediment transport in the Malvinas Current region, western Argentine Basin

We analysed the alkenone unsaturation ratio (U^K′₃₇) in 87 surface sediment samples from the western South Atlantic (5°N–50°S) in order to evaluate its applicability as a paleotemperature tool for this part of the ocean. The measured U^K′₃₇ ratios were converted into temperature using the global core-top calibration of Müller et al. (1998) and compared with annual mean atlas sea-surface temperatures (SSTs) of overlying surface waters. The results reveal a close correspondence (<1.5°C) between atlas and alkenone temperatures for the Western Tropical Atlantic and the Brazil Current region north of 32°S, but deviating low alkenone temperatures by −2° to −6°C are found in the regions of the Brazil–Malvinas Confluence (35–39°S) and the Malvinas Current (41–48°S). From the oceanographic evidence these low U^K′₃₇ values cannot be explained by preferential alkenone production below the mixed layer or during the cold season. Higher nutrient availability and algal growth rates are also unlikely causes. Instead, our results imply that lateral displacement of suspended particles and sediments, caused by strong surface and bottom currents, benthic storms, and downslope processes is responsible for the deviating U^K′₃₇ temperatures. In this way, particles and sediments carrying a cold water U^K′₃₇ signal of coastal or southern origin are transported northward and offshore into areas with warmer surface waters. In the northern Argentine Basin the depth between displaced and unaffected sediments appears to coincide with the boundary between the northward flowing Lower Circumpolar Deep Water (LCDW) and the southward flowing North Atlantic Deep Water (NADW) at about 4000 m.     

D–H evidence for the timing of kaolinization in Northeast Bavaria, Germany

The δD_SMOW values of sedimentary kaolins from the western border of the Bohemian Massif, northeast Bavaria, that did not suffer a deep burial (less than 1000 m) nor a hydrothermal overprint, change systematically from Late Triassic (−50‰) to Mid-Jurassic and Late Cretaceous (−56‰ to −66‰) to Upper Oligocene–Mid-Miocene (−77‰ to −90‰). All analyzed clays are far from hydrogen isotope equilibrium with present-day meteoric waters. Combined oxygen and hydrogen isotope data of selected samples indicate low temperatures of formation (<30°C) and no evidence for preferential D/H exchange with younger waters. The hydrogen isotopic evolution of kaolins is interpreted as reflecting a systematic isotopic change of paleo-meteoric waters in that region. This can be related mainly to the northward drift of stable Europe after the break-up of Gondwana. Increasing continentality, surface uplift and global cooling are additional factors responsible for decreasing δD_SMOW values since the Mid-Cretaceous.

Kaolinite hydrogen isotope ratios of two large residual economic deposits (Tirschenreuth: δD_SMOW=−80‰ to −76‰; Hirschau–Schaittenbach: δD_SMOW=−70‰ to −63‰) can be used in combination with additional geological evidence to constrain the timing of weathering in these areas. A late Early Cretaceous kaolinization age is suggested for the Early Triassic sandstone-hosted deposits near Hirschau–Schnaittenbach, whereas a Late Oligocene to Mid-Miocene age is indicated for the Carboniferous granite-hosted Tirschenreuth deposits.     

Latching hook for instrument retrieval

A light-weight, latching hook on a tapered-strength, light-weight pole retrieves delicate instruments from the sea. The pole is capable of extending the operator's reach more than 6 m in securing a lifting line to instruments more massive than 500 kg.     

CINRAD/SA天气雷达灯丝电源改进电路

针对SA雷达发射机灯丝电源在实际应用过程中进行了跟踪,对出现的电源驱动电路板被烧焦的故障原因和处理办法进行了阐述。现有的SA雷达发射机灯丝电源存在保护性设计缺陷,经常出现破坏性的故障,特别是电源在驱动信号不稳的情况下,两个半桥驱动开关管被击穿,引起驱动电流过大,并烧焦电路板。通过对电路实际维修以及分析,发现此问题是可以克服的,只要适当增加灯丝电源的自我保护功能,并对控制电路进行部分改进,在驱动信号不稳引起电源输出异常时,电源快速收到雷达系统发出的响应信号,自动掐断强电电源,阻止了大电流在驱动信号非稳定期持续经过驱动电路,减少对开关管的冲击,避免随后产生破坏性故障。改进后灯丝电源在部分雷达上进行试用,效果非常理想。     

基于ARMA模型判别气压传感器故障

我国现有的自动气象站设备缺乏能够反映其自身运行状态的参数信息,导致对设备运行监控能力不足,无法快速定位设备故障。为了判别气压传感器的工作状态,从观测数据出发,提出了基于ARMA模型的气压预测方法,利用已测气压值,对当前时刻气压值进行合理的预测,并给出该预测值的置信区间。利用气压传感器的实测值与此预测值进行比较,如果实测值偏离了该预测值的置信区间,可以认为气压传感器或相关数据采集单元出现故障。通过实例计算和比较,模型ARMA(2,1)对于自动气象站气压值的一步预测误差为0,具有较好的预测效果,可以有效判别气压传感器的工作状态。     

基于深度学习的立体影像密集匹配方法综述

三维重建可用于数字高程模型制作、机器人导航、增强现实和自动驾驶等.视差图是三维重建中一种重要的表达方式,而立体密集匹配是使用最广泛的获取视差图的技术.近年来,随着硬件、数据集、算法的发展,基于深度学习的立体匹配方法受到了广泛关注并取得了巨大成功.然而,这些方法通常在近景立体像对中进行测试,很少被用于遥感影像中.回顾了双...