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Presentación en la Segunda Conferencia Subregional del Cono Sur del Consorcio Latinoamericano contra el Aborto Inseguro (CLACAI. Buenos Aires, 4 y 5 de noviembre de 2013.

Tendência temporal e distribuição espacial do aborto inseguro no Brasil, 1996-2012

OBJETIVO: Analisar tendências temporais e padrões de distribuição espacial do aborto inseguro no Brasil. MÉTODOS: Estudo ecológico realizado com base nos registros das internações hospitalares de mulheres por abortamento no Brasil, no período de 1996-2012, obtidos do Sistema de Informações Hospitalares do Ministério da Saúde. Estimou-se o número de abortos inseguros segundo local de residência, utilizando-se técnicas de estimativas indiretas. Foram calculados os indicadores: razão de aborto inseguro por 100 nascidos vivos e coeficiente de aborto inseguro por 1.000 mulheres em idade fértil. As tendências temporais foram analisadas por regressão polinomial e a distribuição espacial utilizando os municípios brasileiros como unidade de análise. RESULTADOS: Foram registradas 4.007.327 internações hospitalares por abortamento no Brasil no período. Estimou-se um total de 16.905.911 abortos inseguros, com média anual de 994.465 abortos (coeficiente médio de aborto inseguro de 17,0 abortos/1.000 mulheres em idade fértil e razão de 33,2 abortos inseguros/100 nascidos vivos). O aborto inseguro apresentou tendência de declínio em nível nacional (R2: 94,0%; p < 0,001), com padrões desiguais entre as regiões. As regiões Nordeste (R2: 93,0%; p < 0,001), Sudeste (R2: 92,0%; p < 0,001) e Centro-Oeste (R2: 64,0%; p < 0,001) apresentaram tendência de declínio, enquanto a região Norte (R2: 39,0%; p = 0,030), tendência de aumento, e a região Sul (R2: 22,0%; p = 0,340), de estabilidade. A análise espacial identificou a presença de clusters de municípios com altos valores de abortos inseguros, localizados especialmente em estados das regiões Norte, Nordeste e Sudeste. CONCLUSÕES: O aborto inseguro se mantém como problema de saúde pública no Brasil, com marcantes diferenças regionais e concentradas nas regiões socioeconomicamente menos favorecidas do País. A qualificação da atenção à saúde da mulher, em especial aos aspectos reprodutivos e de atenção aos processos pré e pós-abortamento, são estratégias necessárias e urgentes.

Horizontal profiles of longwave and shortwave radiation components over sea ice near Barrow, Alaska during the 2011 melt

An integrated instrument package for measuring and understanding the surface radiation budget of sea ice is presented, along with results from its first deployment. The setup simultaneously measures broadband fluxes of upwelling and downwelling terrestrial and solar radiation (four components separately), spectral fluxes of incident and reflected solar radiation, and supporting data such as air temperature and humidity, surface temperature, and location (GPS), in addition to photographing the sky and observed surface during each measurement. The instruments are mounted on a small sled, allowing measurements of the radiation budget to be made at many locations in the study area to see the effect of small-scale surface processes on the large-scale radiation budget. Such observations have many applications, from calibration and validation of remote sensing products to improving our understanding of surface processes that affect atmosphere-snow-ice interactions and drive feedbacks, ultimately leading to the potential to improve climate modelling of ice-covered regions of the ocean. The photographs, spectral data, and other observations allow for improved analysis of the broadband data. An example of this is shown by using the observations made during a partly cloudy day, which show erratic variations due to passing clouds, and creating a careful estimate of what the radiation budget along the observed line would have been under uniform sky conditions, clear or overcast. Other data from the setup's first deployment, in June 2011 on fast ice near Point Barrow, Alaska, are also shown; these illustrate the rapid changes of the radiation budget during a cold period that led to refreezing and new snow well into the melt season.

Concentration and isotope composition of sulphur in sediments and pore water at DSDP Leg 70 Holes

Data obtained while investigating the mounds area near the Galapagos Spreading Center demonstrate the direct influence of solutions derived from the interaction of seawater and young oceanic crust on the sedimentary cover. Investigation of metalliferous sediments from the mid-oceanic ridges, the Galapagos mounds, and the FAMOUS-area zone formations have shown that this influence and the resulting products are dependent on composition, temperature, and conditions of solution input. The study of sulfur in upwardly migrating solutions and the interaction of these solutions with sediments is of great interest. Investigations of different types of hydrothermally derived formations (Edmond, et al., 1979; Spiess et al., 1980; Styrt et al., 1981; Rosanova 1976; Grinenko et al., 1978) have shown the significant role of sulfur-bearing minerals in deposits formed from hightemperature solutions. In contrast, the addition of hydrothermal sulfur is negligible in those metalliferous sediments that precipitated as a result of the interaction between the solutions and open seawater (Bonatti et al., 1972, 1976; Gordeev et al., 1979; Migdisov, Bogdanov, et al., 1979). For example, sulfides are absent in clearly oxidized metalliferous sediments from the East Pacific Rise (EPR). Barite sulfur from these sediments is identical with seawater sulfate sulfur in isotope composition (Grinenko et al., 1978). Gurvich and Bogdanov (1977) have suggested that barium from EPR metalliferous sediments results completely from biological activity and from the components of ocean waters. Edmond et al. (1979) report that low-temperature springs from the Galapagos Rift axis contain two types of solutions: those with and those without H2S.