Granulometry of two sediment cores from Maxwell Bay, South Shetland Islands, West Antarctica

The climate evolution of the South Shetland Islands during the last c. 2000 years is inferred from the multiproxy analyses of a long (928 cm) sediment core retrieved from Maxwell Bay off King George Island. The vertical sediment flux at the core location is controlled by summer melting processes that cause sediment-laden meltwater plumes to form. These leave a characteristic signature in the sediments of NE Maxwell Bay. We use this signature to distinguish summer and winter-dominated periods. During the Medieval Warm Period, sediments are generally finer which indicates summer-type conditions. In contrast, during the Little Ice Age (LIA) sediments are generally coarser and are indicative of winter-dominated conditions. Comparison with Northern and Southern Hemisphere, Antarctic, and global temperature reconstructions reveals that the mean grain-size curve from Maxwell Bay closely resembles the curve of the global temperature reconstruction. We show that the medieval warming occurred earlier in the Southern than in the Northern Hemisphere, which might indicate that the warming was driven by processes occurring in the south. The beginning of the LIA appears to be almost synchronous in both hemispheres. The warming after the LIA closely resembles the Northern Hemisphere record which might indicate this phase of cooling was driven by processes occurring in the north. Although the recent rapid regional warming is clearly visible, the Maxwell Bay record does not show the dominance of summer-type sediments until the 1970s. Continued warming in this area will likely affect the marine ecosystem through meltwater induced turbidity of the surface waters as well as an extension of the vegetation period due to the predicted decrease of sea ice in this area.

Solar irradiance over and under seasonal land-fast sea ice off Barrow, Alaska, in 2010

The amount of solar radiation transmitted through Arctic sea ice is determined by the thickness and physical properties of snow and sea ice. Light transmittance is highly variable in space and time since thickness and physical properties of snow and sea ice are highly heterogeneous on variable time and length scales. We present field measurements of under-ice irradiance along transects under undeformed land-fast sea ice at Barrow, Alaska (March, May, and June 2010). The measurements were performed with a spectral radiometer mounted on a floating under-ice sled. The objective was to quantify the spatial variability of light transmittance through snow and sea ice, and to compare this variability along its seasonal evolution. Along with optical measurements, snow depth, sea ice thickness, and freeboard were recorded, and ice cores were analyzed for chlorophyll a and particulate matter. Our results show that snow cover variability prior to onset of snow melt causes as much relative spatial variability of light transmittance as the contrast of ponded and white ice during summer. Both before and after melt onset, measured transmittances fell in a range from one third to three times the mean value. In addition, we found a twentyfold increase of light transmittance as a result of partial snowmelt, showing the seasonal evolution of transmittance through sea ice far exceeds the spatial variability. However, prior melt onset, light transmittance was time invariant and differences in under-ice irradiance were directly related to the spatial variability of the snow cover.

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.

Sedimentary mineralogy of argillaceous sediments at DSDP Legs 56-57 Holes

Mineral assemblages of DSDP Holes 436 and 438A and the upper section of Hole 439 (871.5-911.0 m sub-bottom) resemble each other and are composed of montmorillonite (probably a small portion of montmorillonite/illite mixed-layer clays), illite, chlorite, kaolinite, quartz, plagioclase, hornblende, calcite, dolomite, siderite, gypsum, pyrite, and halite. In the middle section of Hole 439 (933.5-1041.0 m), clinoptilolite is also found. In the lower section of Hole 439 (1077.5-1150.0 m), montmorillonite is not confirmed, and clinoptilolite and mixed-layer illite are found. These assemblages, which also contain detrital kaolinite, are generally found in sediments from brackish-water environments. At Site 439, more than 1000 meters of sediment might have been removed by erosion at the base.