日本通信综合研究所的时频研究     

孙宏伟 《时间频率学报》1999,22(2):118-122

1996年以来 ,日本通信综合研究所 (简称CRL)在时频方面的研究取得了显著的成绩。其中主要包括 :光抽运铯频标的研制 ;亚太地区卫星双向时间比对网的构造 ;长波授时台的建立。此外还阐述了该所的其他一些时频研究活动  相似文献   

  总被引：2，自引：0，他引：2  

S. E. Kattis  D. Polyzos  D. E. Beskos 《Soil Dynamics and Earthquake Engineering》1999,18(1):78

The three-dimensional problem of isolation of vibration by a row of piles is studied numerically on the basis of a model replacing the row of piles by an effective trench in order to reduce the modelling complexity. The analysis is accomplished with the aid of an advanced frequency domain boundary element method, which is used for both the infilled trench and the soil medium in conjunction with a coupling procedure based on enforcement of equilibrium and compatibility at the trench–soil interface. Linear elastic or viscoelastic material behaviour is assumed for both the piles and the soil. The piles can be tubular or solid and have circular or square cross-section. The vibration source is a vertical force, harmonically varying with time, and the row of piles acts as a passive wave barrier. The effective trench model is constructed by invoking well known homogenization techniques used in the mechanics of fibre-reinforced composite materials, and its accuracy is compared against a rigorous boundary element analysis modelling each pile separately in full contact with the soil medium. On the basis of the effective trench model, the screening effectiveness of a row of piles is studied through parametric studies.  相似文献   

新方法、新理论为太湖环境治理和生态修复提供科技支撑     

唱彤  郦建强  陈文学  郭旭宁  刘为锋  李云玲  吴凤燕 《水科学进展》2024,32(6):1005-1020

全球范围内湖泊富营养化日益严重,影响水资源可持续利用,导致生态系统功能退化,威胁社会经济可持续发展和生态安全。本文系统综述了稳态转换、营养盐控制、生物操纵和环境基准等湖泊系统修复基础理论和最新研究进展;结合国内外湖泊修复实践,对内外源污染物削减、生物措施、水利措施等修复技术方法进行概述。湖泊修复是一项长期艰巨的任务,针对目前尚未解决的问题和新的变化环境,提出科学建立修复目标、营养盐阈值确定、水生生物群落定量关系、流域管控体系建立等研究展望,以期为湖泊修复提供科学支撑。

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基于MODIS影像的超分辨率重建     

丁怡  舒宁  龚衍 《测绘信息与工程》2006,31(1):8-10

针对4幅多时相250 m分辨率的MODIS影像,利用空间域中的超分辨率重建模型,进行了影像的匹配和运动参数估计,重建出采样率提高2倍的高分辨率影像。  相似文献   

Relating a recruitment shift of Patagonian grenadier (Macruronus magellanicus Lönnberg) to large-scale environmental changes off Southern Chile     

LA Cubillos  EJ Niklitschek  S Cahuin 《新西兰海洋与淡水研究杂志》2013,47(2):284-293

The SE Pacific stock of Patagonian grenadier (Macruronus magellanicus) showed evidence of an abrupt reduction in recruitment after 2000. This drop exceeded expectations from changes in the spawning stock biomass (SSB), indicating a change in the stock-recruitment relationship (S-R). We evaluated whether variability in recruitment could be explained by concurrent changes in three environmental indices: sea-surface temperature anomaly (SSTA); southern oscillation index (SOI); and latitudinal position of the west wind drift bifurcation (WWDL). Continuous and discrete effects of these indices were tested as covariates in linear log-log and non-linear Ricker's S-R models. Discrete effects represented regime shifts detected in SSTA (1998), SOI (1998) and WWDL (1995). While SSTA was the only continuous variable found to be significant, the discrete 1998 regime shift supported the most informative model. The best Ricker's model considered a discrete intercept change in the same year: 1998. Although a spurious correlation between SSTA and S-R changes is possible, SSTA may be reflecting major physical or biological changes relevant to M. magellanicus juveniles in the SE Pacific.  相似文献   

    

E. Wielandt 《Geophysical Journal International》1993,113(1):45-53

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黄河银川平原段河岸摆动速率变化及其影响因素(英文)     

王随继  李玲  程维明 《地理学报(英文版)》2014,(4)

It is important to examine the lateral shift rate variation of river banks in different periods. One of the challenges in this regard is how to obtain the shift rate of river banks, as gauging stations are deficient for the study of river reaches. The present study selected the Yinchuan Plain reach of the Yellow River with a length of 196 km as a case study, and searched each point of intersection of 153 cross-sections(interval between two adjacent cross-sections was 1.3 km) and river banks in 1975, 1990, 2010 and 2011, which were plotted according to remote sensing images in those years. Then the shift rates for the points of intersection during 1975–1990, 1990–2010 and 2010–2011 were calculated, as well as the average shift rates for different sections and different periods. The results show that the left bank of the river reach shifts mostly to the right, with the average shift rates being 36.5 m/a, 27.8 m/a and 61.5 m/a in the three periods, respectively. Contemporarily, the right bank shifts mostly to the right in the first period, while it shifts to the left in the second and third periods, with the average shift rates being 31.7 m/a, 23.1 m/a and 50.8 m/a in the three periods, respectively. The average shift rates for the left and right banks during the period 1975–2011 are 22.3 m/a and 14.8 m/a, respectively. The bank shift rates for sections A, B and C are different. The shift rate ratio of the left bank in the three sections is 1:7.6:4.6 for shift to the left and 1:1.7:3.8 for shift to the right, while that of the right bank is 1:1.8:1.2 for shift to the left and 1:5.6:17.7 for shift to the right during the period 1975–2011. Obviously, the average shift rate is the least in section A, while it is maximum in section B for shift to the left and in section C for shift to the right. The temporal variation of the shift rate is influenced by human activities, while the spatial variation is controlled by the local difference in bank materials.  相似文献   

北太平洋维多利亚模态（VM）与海洋性大陆秋季降水年际关系的年代际变化     

朱科旭  任保华  郑建秋 《大气科学》2024,23(4):1444-1456

本文利用HadISST和ERSSTv5海表温度、EN4次表层海温数据、CMAP降水和ERA5再分析资料,研究了北太平洋春季海表温度与海洋性大陆秋季降水年际变化之间的关系及年代际变化特征。研究表明：（1）北太平洋维多利亚模态（VM）是北太平洋春季海表温度EOF第二模态,其与秋季海洋性大陆的降水存在显著的负相关关系。（2）春季的VM为正（负）位相时,通常伴随太平洋经向模态的正（负）位相和西北太平洋的冷（暖）海表温度异常,海表温度梯度会导致赤道太平洋的西风（东风）异常,影响东传的赤道开尔文波,在赤道中东太平洋形成暖（冷）海温异常,再通过Bjerknes正反馈,西风异常和赤道中东太平洋的海温异常维持到秋季,秋季时出现较成熟的厄尔尼诺（拉尼娜）事件。再通过沃克环流,海洋性大陆出现异常下沉（上升）运动和低层辐散、高层辐合（低层辐合、高层辐散）的环流形势,产生降水负（正）异常。（3）春季的VM和秋季的海洋性大陆降水年际变化的关系在2003年发生了年代际转变,1979～2002年春季VM与秋季降水在年际变化上有显著的负相关,而2004～2020年相关关系转变为不显著。造成这个年代际转变的原因是北太平洋涛动（NPO）在2004～2020年强度减弱、位置移动,导致VM南部海表温度关键区受NPO的影响减弱,从而振幅减弱,使得VM的南部和北部海表温度关键区的经向梯度减弱,VM强度减弱,最终导致相关系数降低。  相似文献   

天气雷达网络的进展          下载免费PDF全文

吴琼  仰美霖  陈林  尹红刚  商建  谷松岩 《气象学报》2023,27(2):353-360

通过结合全球降水测量卫星（GPM）反演算法中用到的0℃层亮带模型以及米散射计算,生成了固态、液态以及混合相态3种降水情况下的散射函数查算表;通过与GPM实测数据的对比,验证了查算表的精度,表明散射计算的最大偏差小于0.5 dB。基于该查算表,完成了星载Ku波段雷达到S波段雷达的频率修正。对散射函数的分析表明：Ku波段到S波段的频率修正取决于相态以及谱参数（相似文献   

Damage to surface structures due to underground coal mine blasting: apprehension or real cause?     

P. K. Singh  M. P. Roy 《Environmental Geology》2008,53(6):1201-1211

Investigations were carried out at three underground coal mines in India to study the response of surface structures to underground blasting and the likelihood of damage to the structures. The structures in the vicinity of the underground blasting area were single and multistoried residential houses. The amplitudes of vibration due to underground blasting were monitored simultaneously on the ground surface near the foundation of the structures and on various floors of the structures. The vibrations were also monitored near the important surface installations. It was observed that the magnitude of vibration in structures decreased with the increase in the height of the structures. The frequency of blast vibration from underground blasting was higher than the natural frequency of the structures. Little energy was transmitted into the structures, which caused reduction in the vibration level in the structures. The reduction in the vibration levels was up to 45% in the houses. It indicates that the dominant frequency of blast vibration plays an important role in persistence of vibration and its amplification or reduction characteristics in the structures. This paper deals with the effect of the vibrations on structures/houses standing above the blasting faces in underground workings and their potential to likely damage to the structures at different Indian geo-mining conditions.  相似文献