Pentateuque, Hexateuque et historiographie deutéronomiste. Le problème du début et de la fin du livre de Josué

The book of Joshua is in the very center of the recent discussion about the existence of a coherent deuteronomistic redaction in Deut to 2 Kings during the exilic period. This article analyses the beginning (Josh 1.1-9) and the end (Josh 23 and 24) of Josh. Josh 1.1-2,5-7 and chapter 23 belong to the dtr edition. Josh 23 was followed by Judg 2.6ff. During the Persian period, Deuteronomists and priests intended to publish one Law for the whole community. There was probably a discussion whether the Torah should be a Penta- or a Hexateuch. This discussion may explain such a text as Josh 24 which clearly tries to construct an Hexateuch (cf. also Gen. 50.25: Exod 13.19; Josh 24.32). But since the Torah is about foundations, the main theological trends agreed to have its end with the death of Moses.

Streptozotocin induces a shift towards T regulatory cell responses in vivo

Objectives: Streptozotocin (STZ) induced diabetes is currently the most commonly used animalmodel for islet transplantation.However, STZtreatment and the ensuing hyperglycemia were both shown to affect the immune response, including an apparent induction of lymphopenia. The aim of this study was to evaluate the respective effect of STZ and hyperglycemia on the immune system in STZ induced diabetic C57BL/6 mice. Methods: Phenotypes and levels of T and B cells were analyzed by flow cytometry in blood and spleen over time. The effect of hyperglycemia was further characterized by insulin replacement, islet transplantation and by using Rip (rat insulin promoter) DTR (dipheteria tocin receptor) transgenic mice. Results: STZ but not hyperglycemia was toxic for splenocytes in vitro, whereas hyperglycemia correlated with diabetes associated blood and spleen lymphopenia in vivo. Moreover, independently of hyperglycemia, STZ lead to a relative increase of T regulatory cells which retained their suppressive capacity in vitro. Conclusion: These data suggest thatSTZand the ensuing acute hyperglycemia have major direct and indirect effects on immune homeostasis. Thus, high caution needs to be exercised in the interpretation of the results of tolerance induction and/or immunosuppressive protocols in STZ-induced diabetes and islet transplantation models.

Uso de traçadores para avaliação da hidrodinâmica de sistemas alagados construídos operando sob condições climáticas tropicais

Sistemas alagados construídos (SACs) são, atualmente, importante opção para o tratamento de resíduos e controle da poluição pontual e difusa. O uso de SACs tem aumentado ano a ano, entretanto o nível de entendimento da hidrodinâmica do processo não tem crescido na mesma proporção. Traçadores fluorescentes apresentam-se como opção na determinação de curvas de distribuição de tempos de residência (DTR) e de parâmetros hidrodinâmicos, como número de dispersão e eficiência hidráulica. A pesquisa foi realizada com o objetivo de avaliar dois corantes (rodamina WT e fluoresceína sódica) na determinação das características hidrodinâmicas de SACs com escoamento subsuperficial, operando em região de clima tropical. Os tempos de residência experimentais (τR) para os SACs variaram entre 4,5 e 5,0 dias, e os parâmetros de modelos teóricos foram obtidos para cada sistema, indicando dispersões muito pequenas. Os SACs, que apresentavam relação comprimento/largura (L/B) de 24/1, comportaram-se como sistemas de escoamento próximo ao pistonado. Embora a massa total adicionada não tenha sido recuperada (a adsorção é um dos mecanismos de perda), a pesquisa indicou que a rodamina WT pode ser utilizada com resultados satisfatórios na avaliação do comportamento hidrodinâmico de SACs.

De un modelo tradicional de concesión a un esquema renovado de app para el desarrollo de proyectos de infraestructura vial en Colombia

En la presente investigación se contrasta el Modelo Tradicional de Concesión con el Renovado Esquema de Asociación Público Privada propuesto por la Ley 1508 de 2011 y sus decretos reglamentarios, para establecer, a partir de puntos de contacto y fuga entre una y otra institución, que existe una verdadera transformación del paradigma; y que, este modelo mejorado de participación privada que cuenta con sus propios rasgos definitorios, se erige en principio, como una solución a las exigencias actuales de los proyectos viales de la Cuarta Generación de Concesiones en Colombia, pero a la vez da apertura al debate para la construcción académica del conocimiento, por su reciente implementación.

Educación legal clínica y litigio estratégico en Iberoamérica.

Esta obra es resultado de investigación sobre dos conceptos de enorme importancia para la educación jurídica en Iberoamérica: la educación legal clínica como modelo pedagógico en construcción y el litigio estratégico como herramienta de incidencia social y política. Se considera que el proceso de construcción de las clínicas en la región es un hito en la educación jurídica iberoamericana y existen evidencias que permiten afirmarlo, ya que se trata de historias paralelas que se fortalecieron por los intercambios de aprendizajes y experiencias a través de las redes. De igual manera se desarrolla el concepto de litigio estratégico o estructural y se examina la forma como inciden en dicha propuesta las alianzas estratégicas. Se pasa luego a una profundización sobre la agenda de las clínicas y los temas prioritarios de Derechos Humanos en Iberoamérica. Examen que se realiza a partir de casos reales que se han trabajado las clínicas. Se concluye en la necesidad del surgimiento de nuevas clínicas y de más proyectos de investigación.

Depth by The Rule

This note corrects a previous treatment of algorithms for the metric DTR, Depth by the Rule.

Evidence of trends in daily climate extremes over southern and west Africa

[ 1] There has been a paucity of information on trends in daily climate and climate extremes, especially from developing countries. We report the results of the analysis of daily temperature ( maximum and minimum) and precipitation data from 14 south and west African countries over the period 1961 - 2000. Data were subject to quality control and processing into indices of climate extremes for release to the global community. Temperature extremes show patterns consistent with warming over most of the regions analyzed, with a large proportion of stations showing statistically significant trends for all temperature indices. Over 1961 to 2000, the regionally averaged occurrence of extreme cold ( fifth percentile) days and nights has decreased by - 3.7 and - 6.0 days/decade, respectively. Over the same period, the occurrence of extreme hot (95th percentile) days and nights has increased by 8.2 and 8.6 days/decade, respectively. The average duration of warm ( cold) has increased ( decreased) by 2.4 (0.5) days/decade and warm spells. Overall, it appears that the hot tails of the distributions of daily maximum temperature have changed more than the cold tails; for minimum temperatures, hot tails show greater changes in the NW of the region, while cold tails have changed more in the SE and east. The diurnal temperature range (DTR) does not exhibit a consistent trend across the region, with many neighboring stations showing opposite trends. However, the DTR shows consistent increases in a zone across Namibia, Botswana, Zambia, and Mozambique, coinciding with more rapid increases in maximum temperature than minimum temperature extremes. Most precipitation indices do not exhibit consistent or statistically significant trends across the region. Regionally averaged total precipitation has decreased but is not statistically significant. At the same time, there has been a statistically significant increase in regionally averaged daily rainfall intensity and dry spell duration. While the majority of stations also show increasing trends for these two indices, only a few of these are statistically significant. There are increasing trends in regionally averaged rainfall on extreme precipitation days and in maximum annual 5-day and 1-day rainfall, but only trends for the latter are statistically significant.

Temperature trends at the Mauna Loa observatory, Hawaii

Observations at the Mauna Loa Observatory, Hawaii, established the systematic increase of anthropogenic CO2 in the atmosphere. For the same reasons that this site provides excellent globally averaged CO2 data, it may provide temperature data with global significance. Here, we examine hourly temperature records, averaged annually for 1977–2006, to determine linear trends as a function of time of day. For night-time data (22:00 to 06:00 LST (local standard time)) there is a near-uniform warming of 0.040 °C yr−1. During the day, the linear trend shows a slight cooling of −0.014 °C yr−1 at 12:00 LST (noon). Overall, at Mauna Loa Observatory, there is a mean warming trend of 0.021 °C yr−1. The dominance of night-time warming results in a relatively large annual decrease in the diurnal temperature range (DTR) of −0.050 °C yr−1 over the period 1977–2006. These trends are consistent with the observed increases in the concentrations of CO2 and its role as a greenhouse gas (demonstrated here by first-order radiative forcing calculations), and indicate the possible relevance of the Mauna Loa temperature measurements to global warming.

The urban cool island phenomenon in a high-rise high-density city and its mechanisms

The urban heat island (UHI) phenomenon has been studied extensively, but there are relatively fewer reports on the so-called urban cool island (UCI) phenomenon. We reveal here that the UCI phenomenon exists in Hong Kong during the day, and is associated with the UHI at night under all wind and cloud conditions. The possible mechanisms for the UCI phenomenon in such a high-rise compact city have been discovered using a lumped urban air temperature model. A new concept of urban cool island degree hours (UCIdh) to measure the UCI intensity and duration is proposed. Our analyses reveal that when anthropogenic heat is small or absent, a high-rise and high-density city experiences a significant daytime UCI effect. This is explained by an intensified heat storage capacity and the reduced solar radiation gain of urban surfaces. However, if anthropogenic heat in the urban area increases further, the UCI phenomenon still exists, yet UCIdh decrease dramatically in a high-rise compact city. In a low-rise, low-density city, the UCI phenomenon also occurs when there is no anthropogenic heat, but easily disappears when there is little anthropogenic heat, and the UHI phenomenon dominates. This probably explains why the UHI phenomenon is often observed, but the UCI phenomenon is rarely observed. The co-existence of urban heat/cool island phenomena implies reduction of the daily temperature range (DTR) in such cities, and its dependence on urban morphology also implies that urban morphology can be used to control the urban thermal environment.