Alcances y limitaciones de la ayuda humanitaria desplegada por organismos internacionales como la FAO, OXFAM y CICR frente a la seguridad alimentaria de la población de indonesia tras el tsunami del océano indico

El presente estudio de caso tiene como objetivo analizar la incidencia de la ayuda humanitaria desplegada por la FAO, OXFAM y CICR frente a la seguridad alimentaria de la población de Indonesia tras el tsunami del Océano Indico. Se defiende, que la ayuda humanitaria desplegada por estos actores incidió frente a la seguridad alimentaria de la población de Indonesia luego del evento natural, al restaurar en cierto grado algunos componentes de dicha seguridad como: acceso y utilización de los alimentos mediante diversas estrategias como los programas de desalinización y restauración de cultivos, entre otros que hacen parte esencial de los procesos de rehabilitación y reconstrucción. Para desarrollar esta investigación, se utilizaran los conceptos de ayuda humanitaria y de seguridad alimentaria. Además, será necesario realizar un diseño documental en el que se incluyan tanto fuentes primarias como secundarias.

Secondary education in Afghanistan : a portray of post-conflict education reconstruction. 'La educación secundaria en Afganistán : un retrato de la reconstrucción de la educación después del conflicto'.

Resumen tomado del autor. Resumen del autor también en inglés. Monográfico titulado: La REEC cumple 10 años. La Educación Comparada entre los siglos (1995-2005)

Children born preterm have high risk for central auditory processing deficits, as indexed by the auditory brain event-related potentials (ERPs). 'Los niños prematuros tienen un alto riesgo de dificultades en el procesamiento auditivo central, evidenciadas mediante los potenciales evocados auditivos'.

Resumen basado en el de la publicación. Resumen en español

Historical reconstruction of the Atlantic Meridional Overturning Circulation from the ECMWF operational ocean reanalysis

A reconstruction of the Atlantic Meridional Overturning Circulation (MOC) for the period 1959–2006 has been derived from the ECMWF operational ocean reanalysis. The reconstruction shows a wide range of time-variability, including a downward trend. At 26N, both the MOC intensity and changes in its vertical structure are in good agreement with previous estimates based on trans-Atlantic surveys. At 50N, the MOC and strength of the subpolar gyre are correlated at interannual time scales, but show opposite secular trends. Heat transport variability is highly correlated with the MOC but shows a smaller trend due to the warming of the upper ocean, which partially compensates for the weakening of the circulation. Results from sensitivity experiments show that although the time-varying upper boundary forcing provides useful MOC information, the sequential assimilation of ocean data further improves the MOC estimation by increasing both the mean and the time variability.

A Possible Influence of Equatorial Winds on the September 2002 Southern Hemisphere Sudden Warming Event

The stratospheric sudden warming in the Southern Hemisphere (SH) in September 2002 was unexpected for two reasons. First, planetary wave activity in the Southern Hemisphere is very weak, and midwinter warmings have never been observed, at least not since observations of the upper stratosphere became regularly available. Second, the warming occurred in a west phase of the quasi-biennial oscillation (QBO) in the lower stratosphere. This is unexpected because warmings are usually considered to be more likely in the east phase of the QBO, when a zero wind line is present in the winter subtropics and hence confines planetary wave propagation to higher latitudes closer to the polar vortex. At first, this evidence suggests that the sudden warming must therefore be simply a result of anomalously strong planetary wave forcing from the troposphere. However, recent model studies have suggested that the midwinter polar vortex may also be sensitive to the equatorial winds in the upper stratosphere, the region dominated by the semiannual oscillation. In this paper, the time series of equatorial zonal winds from two different data sources, the 40-yr ECMWF Re-Analysis (ERA) and the Met Office assimilated dataset, are reviewed. Both suggest that the equatorial winds in the upper stratosphere above 10 hPa were anomalously easterly in 2002. Idealized model experiments are described in which the modeled equatorial winds were relaxed toward these observations for various years to examine whether the anomalous easterlies in 2002 could influence the timing of a warming event. It is found that the 2002 equatorial winds speed up the evolution of a warming event in the model. Therefore, this study suggests that the anomalous easterlies in the 1–10-hPa region may have been a contributory factor in the development of the observed SH warming. However, it is concluded that it is unlikely that the anomalous equatorial winds alone can explain the 2002 warming event.