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21.
基于传递熵和再分析数据,讨论了不同ENSO位相下热带中东太平洋与其上空大气的信息传输,研究结果表明:厄尔尼诺、拉尼娜及中性状态下均是以海洋输出信息、大气输入信息为主导的特征,且海洋和大气输入和输出信息的空间分布型较类似。相对中性状态而言,厄尔尼诺和拉尼娜状态下,海洋和大气输入和输出的信息均较强;拉尼娜状态相比厄尔尼诺状态,海洋与大气输入和输出的信息要稍强。通过重排滑动随机抽样方法分析了热带中东太平洋与其上空大气信息传输强度与海温异常的关系,重点分析了热带中东太平洋与其上空大气信息传输的不对称性。揭示了海洋对大气的信息传输随海温距平的变化可以分为类拉尼娜、类中性状态及类厄尔尼诺3个阶段:类拉尼娜阶段,随着低海温的减弱信息传输逐渐减弱;类中性状态,低海温向高海温的过渡过程,信息传输并不存在显著的变化趋势;类厄尔尼诺,随着高海温的增强信息传输逐渐增强。热带中东太平洋与其上空大气信息传输的不对称性更表现为类拉尼娜和类厄尔尼诺阶段信息传输与海温异常之间建立线性关系的阈值和线性趋势程度的不对称。此外,大气对海洋的信息传输随海温的变化与海洋对大气的信息传输随海温的变化类似,即海洋对大气信息传输较强时,大气对海洋的信息传输同样较强,反之亦然,并且大气对海洋的信息传输随海温的变化同样存在不对称性。 相似文献
22.
Richard A. Reyment 《Mathematical Geology》1981,13(6):523-533
Asymmetric relationships in allochthonous units on both sides of the Strait of Gilbraltar (Spain-Morocco) are analyzed by the graphical technique of Gower (1977). The spatial patterns in the rock distributions of these units are shown to be homologous, thus supporting the hypothesis that both sequences derive from the same tectonic episodes. 相似文献
23.
Analysis of inversion errors of ionospheric radio occultation 总被引：3，自引：0，他引：3
The retrieved electron density profile of ionospheric radio occultation (RO) simulation data can be compared with the background
model value during the simulation and the inversion error can be obtained exactly. This paper studies the inversion error
of ionospheric RO through simulation. The sources of the inversion errors are analyzed. The impacts of measurement errors,
such as the errors in phase measurements and satellite orbits, are very small and can be neglected. The approximation of straight-line
propagation introduces errors at the height of the F1 layer under solar maximum condition. The spherical symmetry approximation
of the electron density distribution is found to be the main source of the inversion error. The statistical results reveal
some characteristics of the inversion errors. (1) The relative error increases with enhanced solar activity. (2) It is larger
in winter than in equinox season, and it is smallest in summer. (3) For all seasons, it is smaller at middle latitude than
at other latitudes. (4) For all seasons and geomagnetic latitudes, it is smaller at daytime than at other times. The NmF2
of the ROs from COSMIC are compared with the measurements of ionosondes, and the relative differences show the same dependencies
on season, geomagnetic latitude and local time, as the relative errors of the simulated ionospheric ROs.
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| Xiaocheng WuEmail: |
24.
The paper investigates the influence of design procedures on the seismic response of multi-storey asymmetric buildings. To
this end, some structures are designed according to methods based on either static or modal analysis, with or without design
eccentricities. The seismic response of these systems is determined by means of inelastic dynamic analyses and the design
is thoroughly examined in order to explain the results of the dynamic analyses. Attention is basically focused on the ability
of design methods to prevent asymmetric buildings from experiencing ductility demands much larger than those of the corresponding
torsionally balanced systems. Numerical analyses underline that while design procedures based on either static or modal analysis
are suitable for the design of torsionally rigid structures only those based on modal analysis lead to the satisfactory performance
of torsionally flexible buildings. Furthermore, the study highlights the qualities of a design method proposed by the Authors.
Its application does not require any explicit calculation of design eccentricities and leads to proper seismic response of
both torsionally rigid and flexible asymmetric buildings. 相似文献
25.
根据观测资料的研究指出春季北极涛动(Arctic Oscillation, AO)对随后冬季厄尔尼诺-南方涛动(El Nino–Southern Oscillation, ENSO)的影响具有明显不对称性。春季AO处于正位相时,它对随后冬季厄尔尼诺(El Nino)事件的影响显著,然而春季AO负位相对随后冬季拉尼娜(La Nina)的影响不明显。本研究分析了30个来自CMIP5的耦合模式对春季AO与随后冬季ENSO不对称性关系的模拟能力。30个CMIP5耦合模式中,只有CNRM-CM5和GISS-E2-H-CC模式能较好地抓住春季AO与冬季ENSO的联系。进一步分析这两个模式中春季AO与冬季ENSO的不对称性关系,发现CNRM-CM5模式能较好地再现春季AO与冬季ENSO的非对称关系,即春季AO正(负)位相会导致赤道中东太平洋出现El Nino(La Nina)型海表温度增暖(冷却)。然而,GISS-E2-H-CC模式的模拟结果显示,春季AO对随后冬季ENSO的影响是对称的。本文随后解释了CNRM-CM5(GISS-E2-H-CC)模式能(不能)模拟出春季AO与冬季ENSO不对称关系的原因。对于CNRMCM5模式,在春季AO正位相年,副热带西北太平洋上空存在明显的异常气旋和正降水异常,正降水异常通过Gill型大气响应对赤道西太平洋异常西风的形成和维持起着重要作用,异常西风通过激发向东传播的暖赤道Kelvin波对随后冬季El Nino事件的发生产生显著的影响;然而,在春季AO负位相年,副热带北太平洋的异常反气旋和负降水异常较弱,导致赤道西太平洋的异常东风不明显,因此,春季AO负异常对随后冬季La Nina的影响不显著。所以,CNRM-CM5模式能够较好地抓住春季AO对随后冬季ENSO事件的非对称性影响。相比之下,对于GISS-E2-H-CC模式,春季AO正(负)位相年副热带西北太平洋上存在显著的正(负)降水异常,通过Gill型大气响应在赤道西太平洋激发出明显的异常西(东)风从而影响随后冬季的El Nino(La Nina)事件。因此,在GISS-E2-H-CC模式中,春季AO对随后冬季ENSO具有对称性影响。另外,模式捕捉春季AO对随后冬季ENSO非对称性影响的能力与模式对春季AO空间结构的模拟能力有一定的联系。 相似文献
26.
Post-earthquake observations show that permanent static and transient dynamic displacements in the near field of shallow faults can be complex and quite different from theoretical predictions for homogeneous half-space. These complexities are associated with many departures from the linear, elastic, homogeneous, and isotropic representations, and include the consequences of complex three-dimensional (3D) geology surrounding faults. In this paper we illustrate these complexities for a two-dimensional (2D) model of shallow strike-slip fault when it is inside, on the border, and outside a sedimentary basin. 相似文献
27.
Ground motions are often scaled to certain convenient target spectra in the response assessment of structures. While uniform hazard spectrum (UHS) is more widely used, conditional mean spectrum (CMS) is recently proposed as a more desirable target for scaling of real accelerograms. In this backdrop, the present study spectrally scales, using wavelets, a set of near-field and far-field ground motions to both the targets, viz., UHS and CMS. Relevance of a set of useful ground motion characteristics, viz., the peak ground acceleration-to-peak velocity ratio (amax/vmax), predominant period (Tp), Arias intensity (Ia), Housner intensity (IH), cumulative absolute velocity (CAV) and significant duration (Td⁎), is reviewed. Influence of ground motion scaling is discussed in terms of possible changes of such identified parameters. Seismic demand of horizontally irregular structures is assessed under both scaled and seed records recognizing strength dependent stiffness. Threshold of the scale factor, shown to have well-correlated with the change of ground motion characteristics, may be as high as ~10 to adequately estimate torsion-induced amplification in asymmetric system without any bias. 相似文献
28.
《Geoforum》2015
This paper engages in a critical assessment of environmental management as a way of rethinking our co-habitation with earthly powers. Focusing on the post-disaster reconstruction of Constitución, a Chilean costal city severely damaged by the 2010 tsunami, we argue that environmental management theory has not fully recognised that, sometimes, we humans confront excessive forces that cannot be diplomatically managed or assumed as manageable objects that will readily accept our invitation to compose a common world.Thinking with Sloterdijk’s notions of atmosphere and immunisation, this paper proposes a theoretical programme to re-frame post-disaster environmental management as the creation of life-enabling membranes to contain, isolate and immunise human existence from indifferent forces such as tsunamis. More specifically, we follow the technopolitical controversies around the design of an anti-tsunami park in Constitución to draw attention towards two crucial moments of this process: the definition of the park’s composition and the debate around the park’s fallibility. We argue that these moments point to a type of environmental management engaged in the articulation of an immunising atmosphere to secure an interior for human dwelling. Moreover, these two moments specify empirical challenges not fully developed in Sloterdijk’s atmospheric philosophy: the rearrangement of science, politics and materials that is brought along in the process of erecting an immunological membrane; and the bioeconomy of life (and death) that emerges upon the possibility of an immunitary breakdown. In the concluding section we turn to the ecological and ethical challenges opened up by an atmospheric approach to environmental management. 相似文献
29.
Enhanced bioturbation on the down‐drift flank of a Turonian asymmetrical delta: Implications for seaway circulation,river nutrients and facies models 
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下载免费PDF全文 Extant models predict delta front environments down‐drift of river mouths as unfavourable for organisms because of the physico‐chemical stresses caused by sediment and fresh water influx. This study, however, finds evidence for near‐optimal living conditions down‐drift of contemporaneous mouth bars and distributary channels, as well as at the tops of abandoned lobes, in part of the asymmetrical ‘Notom Delta’ complex of the Ferron Sandstone (Turonian, south‐eastern Utah, USA). Presented herein is a sedimentological and ichnological model using thirty‐two detailed measured sections along a 16 km transect through two continuously exposed, ca 10 m thick allomembers containing delta front, mouth bar and distributary channel facies. Azimuths from sedimentary structures show south‐eastward deflection of near‐shore palaeocurrents relative to the inferred north–south shoreline, as well as minor reversal of flow. Two end‐member trace fossil suites are recognized in delta front sandstones: (i) a stressed suite of low abundance, low diversity, diminutive traces reflecting mobile deposit feeding, resting and locomotion behaviours; and (ii) a comparatively unstressed, high abundance, moderate diversity suite with a regular, heterogeneous distribution of deep, vertical or U‐shaped suspension‐feeding burrows which, in places, thoroughly homogenize the sandstones. The down‐drift side of the delta was colonized by suspension feeders during seasonal reversal of the seaway gyre when mud plumes were swept northward or when river‐derived nutrients were sufficiently concentrated relative to fresh water and sediment input. During normal seaway circulation, very high sedimentation rates and mud‐laden, wave‐dampened waters down‐drift of the river mouths heightened the preservation potential of the pervasively bioturbated facies. Up‐drift of the river mouths, these bioturbated facies were either not preserved or not developed until the lobe was abandoned. This alternative model for delta planform asymmetry contributes to the refinement of facies models for deltaic systems and provides a framework for predicting the distribution of bioturbation‐enhanced porosity and permeability in lobe‐deflected deltas. 相似文献
30.
热带非稳定波（ＴＩＷｓ）关于赤道的径向不对称是其突出特征之一。本文利用二层半线性海洋模式研究各种不对称背景条件对非稳定波不对称性的影响。结果表明，在大西洋和太平洋上热带非稳定波（ＴＩＷｓ）的不对称性似是由于南赤道流的两个分支和海面温度锋面对于赤道的不对称性，而不是由于北赤道逆流的出现。 相似文献