Impacts of interruption of the Agulhas leakage on the tropical Atlantic in coupled ocean-atmosphere simulations

In this paper we use a coupled ocean-atmosphere model to investigate the impact of the interruption of Agulhas leakage of Indian ocean water on the tropical Atlantic, a region where strong coupled ocean-atmosphere interactions occur. The effect of a shut down of leakage of Indian ocean water is isolated from the effect of a collapse of the MOC. In our experiments, the ocean model is forced with boundary conditions in the southeastern corner of the domain that correspond to no interocean exchange of Indian ocean water into the Atlantic. The southern boundary condition is taken from the Levitus data and ensures an MOC in the Atlantic. Within this configuration, instead of warm and salty Indian ocean water temperature (cold) and salinity (fresh) anomalies of southern ocean origin propagate into the South Atlantic and eventually reach the equatorial region, mainly in the thermocline. This set up mimics the closure of the ""warm water path"" in favor of the ""cold water path"". As part of the atmospheric response, there is a northward shift of the intertropical convergence zone (ITCZ). The changes in trade winds lead to reduced Ekman pumping in the equatorial region. This leads to a freshening and warming of the surface waters along the equator. Especially in the Cold Tongue region, the cold and fresh subsurface anomalies do not reach the surface due to the reduced upwelling. The anomaly signals are transported by the equatorial undercurrent and spread away from the equator within the thermocline. Part of the anomaly eventually reaches the Tropical North Atlantic, where it affects the Guinea Dome. Surprisingly, the main effect at the surface is small on the equator and relatively large at the Guinea Dome. In the atmosphere, the northward shift of the ITCZ is associated with a band of negative precipitation anomalies and higher salinities over the Tropical South Atlantic. An important implication of these results is that the modified water characteristics due to a shut down of the Agulhas leakage remain largely unaffected when crossing the equatorial Atlantic and therefore can affect the deepwater formation in the North Atlantic. This supports the hypothesis that the Agulhas leakage is an important source region for climate change and decadal variability of the Atlantic.

Distribution of major elements in Atlantic surface sediments (36 degrees N-49 degrees S): Imprint of terrigenous input and continental weathering

Numerous studies use major element concentrations measured on continental margin sediments to reconstruct terrestrial climate variations. The choice and interpretation of climate proxies however differ from site to site. Here we map the concentrations of major elements (Ca, Fe, Al, Si, Ti, K) in Atlantic surface sediments (36 degrees N-49 degrees S) to assess the factors influencing the geochemistry of Atlantic hemipelagic sediments and the potential of elemental ratios to reconstruct different terrestrial climate regimes. High concentrations of terrigenous elements and low Ca concentrations along the African and South American margins reflect the dominance of terrigenous input in these regions. Single element concentrations and elemental ratios including Ca (e. g., Fe/Ca) are too sensitive to dilution effects (enhanced biological productivity, carbonate dissolution) to allow reliable reconstructions of terrestrial climate. Other elemental ratios reflect the composition of terrigenous material and mirror the climatic conditions within the continental catchment areas. The Atlantic distribution of Ti/Al supports its use as a proxy for eolian versus fluvial input in regions of dust deposition that are not affected by the input of mafic rock material. The spatial distributions of Al/Si and Fe/K reflect the relative input of intensively weathered material from humid regions versus slightly weathered particles from drier areas. High biogenic opal input however influences the Al/Si ratio. Fe/K is sensitive to the input of mafic material and the topography of Andean river drainage basins. Both ratios are suitable to reconstruct African and South American climatic zones characterized by different intensities of chemical weathering in well-understood environmental settings.

Importância dos vírus respiratórios na febre sem sinais localizatórios em crianças menores de 36 meses

INTRODUÇÃO Cerca de 20% das crianças menores de 36 meses trazidas ao setor de emergência por febre apresentam febre sem sinais localizatórios (FSSL). Nos últimos anos, vários estudos estabeleceram critérios para a identificação dos pacientes com risco de infecção bacteriana grave (IBG), além de demonstrarem a aplicabilidade da pesquisa de vírus respiratórios (PVR) na avaliação destes pacientes. Entretanto, não existem estudos abordando a identificação de vírus respiratórios em crianças menores de 36 meses com FSSL no nosso meio. OBJETIVOS Descrever a frequência dos vírus respiratórios na febre sem sinais localizatórios (FSSL) em crianças menores de 36 meses de idade CASUÍSTICA E MÉTODOS Estudo prospectivo e observacional de crianças menores de 36 meses no setor de emergência pediátrico, durante o período de abril de 2011 a abril de 2013, com diagnóstico de FSSL. Foram excluídas crianças portadoras de doenças de base que implicavam em alteração da imunidade e uso de antibiótico até 14 dias antes da consulta. Os pacientes foram avaliados laboratorialmente de acordo com o protocolo institucional para avaliação de FSSL. Além de hemograma completo, análise do sedimento urinário e culturas de sangue e urina, foi coletada amostra de secreção de nasofaringe para pesquisa de vírus respiratórios por imunoflourescência indireta. Resultados Foram estudados 232 crianças menores de 36 meses com diagnóstico de FSSL, sendo 53% do sexo masculino, com idade mediana de 10,7 meses (5,4 - 16,1). Em 57 (24,6%) destes pacientes, foi identificado vírus respiratórios, sendo o adenovírus (33 casos - 57,9%) o agente mais identificado, seguido do parainfluenza 3 (17,5%) e do influenza A (12,3%). CONCLUSÃO Em torno de 25% dos casos de FSSL do nosso meio foram identificados vírus respiratórios, mostrando que a PVR é uma ferramenta útil na avaliação do paciente com FSSL, possibilitando a redução do número de retornos hospitalares e uso de antibioticoterapia empírica.