bluuebunny/crossref_metadata_2025_split huggingface dataset:
Criminal Justice in Asia and Japan and the International Criminal Court
Authors: Noguchi Motoo 
Published: November 2006

AbstractThe under-representation of Asia in the International Criminal Court is an issue of serious concern. This article addresses criminal justice in Asia and Japan, hoping to help enhance the understanding of their special circumstances and assist in increasing the number of State Parties to the ICC. More specifically, it (i) identifies common features surrounding society and culture in many Asian countries that are hindrances or possible reasons why they haven't acceded; (ii) discusses the main characteristics of the Japanese criminal investigation and trial system that reflect the influence of both the civil law and common law legal systems; (iii) gives a brief overview of the history of the development of the Japanese criminal law since the late 19th century; (iv) touches upon some of the main legal issues that Japan needs to consider before acceding to the Statute; and (v) clarifies the significance of Japan becoming a State Party.
Anthropology in the 'Integral Depth Ecology' of Jochen Kirchhoff
Authors:   Krüger
Published: November 2006

AbstractThis article provides a structural analysis of the position of the human being (anthropos) in the integrale Tiefenökologie of the philosopher Jochen Kirchhoff (born 1944). This term denotes not only the indissoluble unity of human and cosmos, but also the entire spectrum of consciousness, from the physical level of matter/energy to the transpersonal level of Spirit/the Absolute, in an epistemological as well as ontological sense. The contours of the ecological problem, according to Kirchhoff, as well as the outlines of his remedial project are drawn, in the context of the tradition in which he stands and the contemporary discourse (modern science) from which he disengages himself.
Cognitive Science, Ritual, and the Hellenistic Mystery Religions
Authors: Martin Luther 
Published: November 2006

AbstractMuch research in the cognitive science of religion has dealt with ritual. Two forms of ritual have been focused on, those characterised by repetition and routinisation, the characteristic most often attributed ritual, and the less noted forms in which ritual performance is infrequent and irregular but highly emotional and arousing. I hope, in this essay, to suggest the utility of cognitive theorising for the historical study of ritual with examples from the religions of the Roman Empire, especially, the Hellenistic Mystery Religions and the early Christianities, and to arouse interest in pursuing such studies further in the history of religions.
The Evil of Violence: A Trigger for a Human Rights Culture?
Authors: Pieterse Hendrik , Dreyer Jaco , van der Ven Johannes 
Published: November 2006

AbstractThis article seeks to answer the following question: to what extent does the interpretation of violence as evil contribute – positively, negatively or not at all – to a human rights culture among some 2000 grade 11 students at private (Catholic and Anglican) schools and Afrikaans medium public schools in the Johannesburg/Pretoria region on the basis of surveys conducted in 1995/1996 and 2000/2001? The regression analyses show that on a number of population characteristics controlled hamartiological interpretations of violence as evil have a mainly positive effect, especially those couched in terms of the divine apocalypse, provided it is construed in its positive dimension ('the new Jerusalem') rather than its negative dimension ('the last judgment'); this also applies to interpretations couched in terms of the institutional transmission of evil contributing to the world of evil. The other interpretations have a predominantly or purely negative effect, especially those relating to a primordial dualistic struggle between good and evil forces, divine retribution and intergeneration transmission of evil. Some population characteristics appear to be more powerful than the hamartiological interpretations, especially gender (female students are more in favour of human rights) and political and cultural attitudes.
Norwegian Ecclesiastical Affiliation in Three Countries: a Challenge to Earlier Historiography
Authors: Hale Frederick 
Published: November 2006

AbstractHistorians like Oscar Handlin and Timothy L. Smith asserted that international migration, especially that of Europeans to North America, was a process which reinforced traditional religious loyalties. In harmony with this supposed verity, a venerable postulate in the tradition of Scandinavian-American scholarship was that most Norwegian immigrants in the New World (the overwhelming majority of whom had been at least nominal members of the Evangelical Lutheran Church of Norway) clung to their birthright religious legacy and affiliated with Lutheran churches after crossing the Atlantic (although for many decades it has been acknowledged that by contrast, vast numbers of their Swedish-American and Danish-American counterparts did not join analogous ethnic Lutheran churches). In the present article, however, it is demonstrated that anticlericalism and alienation from organised religious life were widespread in nineteenth-century Norway, where nonconformist Christian denominations were also proliferating. Furthermore, in accordance with these historical trends, the majority of Norwegian immigrants in the United States of America and Southern Africa did not affiliate with Lutheran churches. Significant minorities joined Baptist, Methodist, and other non-Lutheran religious fellowships, but the majority did not become formally affiliated with either Norwegian or pan-Scandinavian churches.
A Study of Cloud Mixing and Evolution Using PDF Methods. Part I: Cloud Front Propagation and Evaporation
Authors: Jeffery Christopher A. , Reisner Jon M. 
Published: November 2006

AbstractThe evolution of mean relative humidity (RH) is studied in an isobaric system of clear and cloudy air mixed by an incompressible velocity field. A constant droplet radius assumption is employed that implies a simple dependence of the mixing time scale, τeddy, and the reaction (evaporation) time scale, τreact, on the specifics of the droplet size spectrum. A dilemma is found in the RH e-folding time, τefold, predicted by two common microphysical schemes: models that resolve supersaturation and ignore subgrid correlations, which gives τefold ∼ τreact, and PDF schemes that assume instantaneous evaporation and predict τefold ∼ τeddy. The resolution of this dilemma, Magnussen and Hjertager’s eddy dissipation concept (EDC) model τefold ∼ max(τeddy, τreact), is revealed in the results of 1D eddy diffusivity simulations and a new probability density function (PDF) approach to cloud mixing and evolution in which evaporation is explicitly resolved and the shape of the PDF is not specified a priori. The EDC model is shown to exactly solve the nonturbulent problem of spurious production of cloud-edge supersaturations described by Stevens et al. and produce good results in the more general turbulent case.
Classification of Ice Crystal Shapes in Midlatitude Ice Clouds from Three Years of Lidar Observations over the SIRTA Observatory
Authors: Noel Vincent , Chepfer Helene , Haeffelin Martial , Morille Yohann 
Published: November 2006

Abstract
This paper presents a study of ice crystal shapes in midlatitude ice clouds inferred from a technique based on the comparison of ray-tracing simulations with lidar depolarization ratio measured at 532 nm. This technique is applied to three years of lidar depolarization ratio observations from the Site Instrumental de Recherche par Télédétection Atmosphérique (SIRTA) observatory in Palaiseau, France, amounting to 322 different days of ice cloud observations. Particles in clouds are classified in three major groups: plates, columns, and irregular shapes with aspect ratios close to unity. Retrieved shapes are correlated with radiosounding observations from a close-by meteorological station: temperature, relative humidity, wind speed, and direction.
Results show a strong dependence of the relative concentration of different crystal shapes to most atmospheric variables, such as the temperature, with a clear successive dominance by platelike (temperature above −20°C), irregular (temperatures between −60° and −40°C), and columnlike shapes (temperatures below −60°C). Particle shapes are almost exclusively columnlike below −75°C. This is in sharp contrast with previous results of the same classification applied to tropical clouds, and highlights the high geographic variability of the ice clouds distribution of microphysical properties. Results also suggest that ice clouds created by jet streams (identified by high wind speeds) are strongly dominated by columnlike shapes, while front-created ice clouds (identified by lower wind speeds) show a much more variable mix of shapes, with the dominant shapes depending on other factors. Results also suggest different microphysical properties according to the average direction source of air masses and winds. Following these results, a possible parameterization of ice crystal shapes in midlatitude ice clouds as a function of temperature is provided.
Two-Dimensional Spectra in the Atmospheric Boundary Layer
Authors: Kelly Mark , Wyngaard John C. 
Published: November 2006

AbstractOne-dimensional spectra are frequently used to relate features of measured and simulated meteorological field variables in the turbulent atmospheric boundary layer (ABL), but two-dimensional spectra can provide more reliable scale information than one-dimensional spectra. Here a method is presented for obtaining two-dimensional spectra from one-dimensional spectra, and it includes examples using data from large-eddy simulations and field measurements in the ABL.
The Role of Land–Sea Topography in Blocking Formation in a Block–Eddy Interaction Model
Authors: Luo Dehai , Chen Zhe 
Published: November 2006

Abstract
This paper is an extension of a theoretical study by Luo on the effect of large-scale land–sea contrast (LSC) topography on the formation of an eddy-driven blocking. It is found that the topography term can be included explicitly in the blocking evolution equation because of the inclusion of the higher-order wave–topography interaction. Although the blocking flow cannot be excited purely by the LSC topography, the LSC topography is found to be capable of enhancing the amplification of the dipole component in a blocking flow associated with upstream synoptic-scale eddies. In this case, a strong omega-type blocking high can be driven by the joint action of synoptic-scale eddies and LSC topography. This seems to provide an explanation of a difference in blocking intensity between the Northern and Southern Hemispheres. The most important finding of this paper is that in the presence of LSC topography the double jets that appear during the onset of an eddy-driven dipole block collapse into a strong single westerly jet that is within the south side of an omega-type blocking high, which is different from the result predicted by the theoretical model proposed in Luo’s previous work.
Exploring Self-Correlation in Flux–Gradient Relationships for Stably Stratified Conditions
Authors: Baas P. , Steeneveld G. J. , van de Wiel B. J. H. , Holtslag A. A. M. 
Published: November 2006

Abstract
In this paper, the degree of scatter in flux–gradient relationships for stably stratified conditions is analyzed. It is generally found that scatter in the dimensionless lapse rate ϕh is larger than in the dimensionless shear ϕm when plotted versus the stability parameter z/Λ (where Λ is the local Obukhov length). Here, this phenomenon is explained to be a result of self-correlation due to the occurrence of the momentum and the heat flux on both axes, measurement uncertainties, and other possibly relevant physical processes left aside. It is shown that the ratio between relative errors in the turbulent fluxes influences the orientation of self-correlation in the flux–gradient relationships. In stable conditions, the scatter in ϕm is largely suppressed by self-correlation while for ϕh this is not the case (vice versa for unstable stratification). An alternative way of plotting is discussed for determining the slope of the linear ϕm function.
What Is the Shape of a Raindrop? An Answer from Radar Measurements
Authors: Gorgucci Eugenio , Baldini Luca , Chandrasekar V. 
Published: November 2006

AbstractIn a previous study, Gorgucci et al. showed the potential advantage of using together polarimetric radar measurements of reflectivity factor, differential reflectivity, and specific differential propagation phase, in order to gather information about the calibration of radar systems. Scarchilli et al. generalized this concept in the self-consistency principle, which stated that, given a drop-shape model to describe the form of raindrops, the corresponding radar measurements are constrained on this three-dimensional surface. In this work the self-consistency principle is collapsed onto a two-dimensional domain defined by the variables: 1) the ratio between specific differential phase and reflectivity factor, and 2) differential reflectivity. In this space the scatter of drop size distribution (DSD) variability is minimized in such a way that drop-shape variability shows up. This methodology is used to observe for the first time the predominant shape of raindrops directly from the radar measurements. The radar polarimetric data were collected in two different climatological regions as central Florida and northern Italy. The significant result shows that the underlying mean axis ratio approaches the model established by Pruppacher and Beard, and the relationship described by Beard and Chuang forms a sort of border for the sphericity of the drop shape.
Relative Humidity in Liquid, Mixed-Phase, and Ice Clouds
Authors: Korolev Alexei , Isaac George A. 
Published: November 2006

AbstractThe results of in situ observations of the relative humidity in liquid, mixed, and ice clouds typically stratiform in nature and associated with mesoscale frontal systems at temperatures −45°C &lt; Ta &lt; −5°C are presented. The data were collected with the help of instrumentation deployed on the National Research Council (NRC) Convair-580. The length of sampled in-cloud space is approximately 23 × 103 km. The liquid sensor was calibrated in liquid clouds with the assumption that the air in liquid clouds is saturated with respect to water. It was found that the relative humidity in mixed-phase clouds is close to saturation over water in the temperature range from −5° to −35°C for an averaging scale of 100 m. In ice clouds the relative humidity over ice is not necessarily equal to 100%, and it may be either lower or higher than saturation over ice, but it is always lower than saturation over water. On average the relative humidity in ice clouds increases with a decrease of temperature. At −40°C the relative humidity over ice is midway between saturation over ice and liquid. A parameterization for the relative humidity in ice clouds is suggested. A large fraction of ice clouds was found to be undersaturated with respect to ice. The fraction of ice clouds undersaturated with respect to ice increases toward warmer temperatures.
Cloud Properties Simulated by a Single-Column Model. Part II: Evaluation of Cumulus Detrainment and Ice-Phase Microphysics Using a Cloud-Resolving Model
Authors: Luo Yali , Krueger Steven K. , Xu Kuan-Man 
Published: November 2006

Abstract
This paper is the second in a series in which kilometer-scale-resolving observations from the Atmospheric Radiation Measurement Program and output from the University of California, Los Angeles/Colorado State University cloud-resolving model (CRM) are used to evaluate the single-column model (SCM) version of the National Centers for Environmental Prediction Global Forecast System model. Part I demonstrated that kilometer-scale cirrus properties analyzed by applying the SCM’s assumptions about cloud vertical overlap and horizontal homogeneity to its profiles of cloud water/ice mixing ratio, cloud fraction, and snow flux differed from the cloud radar observations while the CRM simulation reproduced most of the observed cirrus properties. The present study evaluates, through a comparison with the CRM, the SCM’s representation of detrainment from deep cumulus and ice-phase microphysics in an effort to better understand the findings of Part I.
This study finds that, although the SCM’s detrainment rate profile averaged over the entire simulation period is comparable to the CRM’s, detrainment in the SCM is comparatively sporadic and vertically localized. Too much detrained ice is sublimated when first detrained. Snow formed from detrained cloud ice falls through too deep of a layer. These aspects of the SCM’s parameterizations may explain many of the differences in the cirrus properties between the SCM and the observations (or between the SCM and the CRM), and suggest several possible improvements for the SCM: 1) allowing multiple coexisting cumulus cloud types as in the original Arakawa–Schubert scheme, 2) prognostically determining the stratiform cloud fraction, and 3) explicitly predicting the snow mixing ratio. These would allow better representation of the detrainment from deep convection, better coupling of the volume of detrained air with cloud fraction, and better representation of snow flux.
Gap Flows through Idealized Topography. Part II: Effects of Rotation and Surface Friction
Authors: Gaberšek Saša , Durran Dale R. 
Published: November 2006

Abstract
Numerical simulations are conducted of geostrophically balanced flow over an isolated mountain cut by a horizontal gap. The relative importance of the along-gap synoptic-scale pressure gradient and terrain-induced mesoscale circulations for the generation of gap winds was examined by changing the direction of the synoptic-scale wind relative to the topography. In all cases, the forcing associated with mesoscale circulations generated by the mountain was at least as significant as the synoptic-scale pressure gradient. In the cases where a component of the large-scale flow was directed perpendicular to the ridge, the dynamics were dominated by either the vertical momentum fluxes due to mountain lee waves or by mesoscale pressure gradients associated with upstream blocking or lee troughing. Mesoscale circulations were also important when the large-scale flow was parallel to the ridge because surface friction turned the low-level winds toward the high pressure side of the ridge, partially blocking the flow and enhancing the along-gap pressure gradient.
The flow in the interior of a very long uniform gap was also simulated for a case with the synoptic-scale winds parallel to the ridge so that the synoptic-scale pressure gradient was down the gap. The flow in the interior of the long gap was not horizontal and not in a simple dynamical balance between acceleration, the pressure gradient force, and surface friction. Even the flow in the lowest 150 m was gradually subsiding. Subsidence and lateral momentum flux convergence at low levels near the center of the gap were important contributors to the mass and along-gap momentum budgets.
Normal-Mode Analysis of a Baroclinic Wave-Mean Oscillation
Authors: Wolfe Christopher L. , Samelson Roger M. 
Published: November 2006

Abstract
The stability of a time-periodic baroclinic wave-mean oscillation in a high-dimensional two-layer quasigeostrophic spectral model is examined by computing a full set of time-dependent normal modes (Floquet vectors) for the oscillation. The model has 72 × 62 horizontal resolution and there are 8928 Floquet vectors in the complete set. The Floquet vectors fall into two classes that have direct physical interpretations: wave-dynamical (WD) modes and damped-advective (DA) modes. The WD modes (which include two neutral modes related to continuous symmetries of the underlying system) have large scales and can efficiently exchange energy and vorticity with the basic flow; thus, the dynamics of the WD modes reflects the dynamics of the wave-mean oscillation. These modes are analogous to the normal modes of steady parallel flow. On the other hand, the DA modes have fine scales and dynamics that reduce, to first order, to damped advection of the potential vorticity by the basic flow. While individual WD modes have immediate physical interpretations as discrete normal modes, the DA modes are best viewed, in sum, as a generalized solution to the damped advection problem. The asymptotic stability of the time-periodic basic flow is determined by a small number of discrete WD modes and, thus, the number of independent initial disturbances, which may destabilize the basic flow, is likewise small. Comparison of the Floquet exponent spectrum of the wave-mean oscillation to the Lyapunov exponent spectrum of a nearby aperiodic trajectory suggests that this result will still be obtained when the restriction to time periodicity is relaxed.
Potential Vorticity Diagnosis of a Simulated Hurricane. Part II: Quasi-Balanced Contributions to Forced Secondary Circulations
Authors: Zhang Da-Lin , Kieu Chanh Q. 
Published: November 2006

Abstract
Although the forced secondary circulations (FSCs) associated with hurricane-like vortices have been previously examined, understanding is still limited to idealized, axisymmetric flows and forcing functions. In this study, the individual contributions of latent heating, frictional, and dry dynamical processes to the FSCs of a hurricane vortex are separated in order to examine how a hurricane can intensify against the destructive action of vertical shear and how a warm-cored eye forms. This is achieved by applying a potential vorticity (PV) inversion and quasi-balanced omega equations system to a cloud-resolving simulation of Hurricane Andrew (1992) during its mature stage with the finest grid size of 6 km.
It is shown that the latent heating FSC, tilting outward with height, acts to oppose the shear-forced vertical tilt of the storm, and part of the upward mass fluxes near the top of the eyewall is detrained inward, causing the convergence aloft and subsidence warming in the hurricane eye. The friction FSC is similar to that of the Ekman pumping with its peak upward motion occurring near the top of the planetary boundary layer (PBL) in the eye. About 40% of the PBL convergence is related to surface friction and the rest to latent heating in the eyewall.
In contrast, the dry dynamical forcing is determined by vertical shear and system-relative flow. When an axisymmetric balanced vortex is subjected to westerly shear, a deep countershear FSC appears across the inner-core region with the rising (sinking) motion downshear (upshear) and easterly sheared horizontal flows in the vertical. The shear FSC is shown to reduce the destructive roles of the large-scale shear imposed, as much as 40%, including its forced vertical tilt. Moreover, the shear FSC intensity is near-linearly proportional to the shear magnitude, and the wavenumber-1 vertical motion asymmetry can be considered as the integrated effects of the shear FSCs from all the tropospheric layers. The shear FSC can be attributed to the Laplacian of thermal advection and the temporal and spatial variations of centrifugal force in the quasi-balanced omega equation, and confirms the previous finding of the development of wavenumber-1 cloud asymmetries in hurricanes.
Hurricane eye dynamics are presented by synthesizing the latent heating FSC with previous studies. The authors propose to separate the eye formation from maintenance processes. The upper-level inward mass detrainment forces the subsidence warming (and the formation of an eye), the surface pressure fall, and increased rotation in the eyewall. This increased rotation will induce an additional vertical pressure gradient force to balance the net buoyancy generated by the subsidence warming for the maintenance of the hurricane eye. In this sense, the negative vertical shear in tangential wind in the eyewall should be considered as being forced by the subsidence warming, and maintained by the rotation in the eyewall.