Climatic variability in Central Indian Himalaya during the last similar to 1800 years: Evidence from a high resolution speleothem record

Stable isotopes from a U/Th dated aragonite stalagmite from the Central Kumaun Himalaya provide evidence of variation in climatic conditions in the last similar to 1800 years. The delta O-18 and delta C-13 values vary from -4.3 parts per thousand to -7.6 parts per thousand and -3.4 parts per thousand to -9.1 parts per thousand respectively, although the stalagmite was not grown in isotopic equilibrium with cave drip water, a clear palaeoclimatic signal in stalagmite delta O-18 values is evident based on the regional climate data. The stalagmite showed a rapid growth rate during 830-910 AD, most likely the lower part of Medieval Warm Period (MWP), and 1600-1640 AD, the middle part of Little Ice Age (LIA). Two distinct phases of reduced precipitation are marked by a 2 parts per thousand shift in 8180 values towards the end of MWP (similar to 1080-1160 AD) and after its termination from similar to 1210 to 1440 AD. The LIA (similar to 1440-1880 AD) is represented by sub-tropical climate similar to modern conditions, whereas the post-LIA was comparatively drier. The Inter Tropical Convergence Zone (ITCZ) was located over the cave location during wetter/warmer conditions. When it shifted southward, precipitation over the study area decreased. A prominent drop in delta O-18 and delta C-13 values during the post-LIA period may also have been additionally influenced by anthropogenic activity in the area. (C) 2013 Elsevier Ltd and INQUA. All rights reserved.

El espacio memorial de los/as desaparecidos/as : algunas perspectivas epistemológicas

Resumen: La pregunta que guía este trabajo está referida a la posibilidad de extraer algunas perspectivas epistemológicas de la producción de un espacio memorial. Su tema está relacionado con los modos de reelaboración del trauma social. El tiempo histórico al que se refiere es el de la última dictadura cívico-militar (marzo 1976-diciembre 1983). El recorrido de este aporte tiene tres partes. En la primera, se consideran las nociones de cuerpo y narración; la segunda presenta esbozos de respuestas a la pregunta planteada y la tercera, está referida brevemente a dos mujeres europeas y cristianas: Alice Domon (Francia, 1937- Argentina, 1977) y Elisabeth Käsemann (Alemania, 1947- Argentina 1977). Ambas vivieron en América Latina y pueden ser consideradas verdaderos espacios humanitarios de paz.

Las adaptaciones fílmicas de los textos clásicos: el caso de "The Last of the Mohicans"

Santamaría, José Miguel; Pajares, Eterio; Olsen, Vickie; Merino, Raquel; Eguíluz, Federico (eds.)

La poesía española bajo el franquismo: compromiso y denuncia

Ejemplar monográfico titulado: "De poesía y crítica"

The deep ocean density structure at the Last Glacial Maximum : What was it and why?

The search for reliable proxies of past deep ocean temperature and salinity has proved difficult, thereby limiting our ability to understand the coupling of ocean circulation and climate over glacial-interglacial timescales. Previous inferences of deep ocean temperature and salinity from sediment pore fluid oxygen isotopes and chlorinity indicate that the deep ocean density structure at the Last Glacial Maximum (LGM, approximately 20,000 years BP) was set by salinity, and that the density contrast between northern and southern sourced deep waters was markedly greater than in the modern ocean. High density stratification could help explain the marked contrast in carbon isotope distribution recorded in the LGM ocean relative to that we observe today, but what made the ocean's density structure so different at the LGM? How did it evolve from one state to another? Further, given the sparsity of the LGM temperature and salinity data set, what else can we learn by increasing the spatial density of proxy records?

We investigate the cause and feasibility of a highly and salinity stratified deep ocean at the LGM and we work to increase the amount of information we can glean about the past ocean from pore fluid profiles of oxygen isotopes and chloride. Using a coupled ocean--sea ice--ice shelf cavity model we test whether the deep ocean density structure at the LGM can be explained by ice--ocean interactions over the Antarctic continental shelves, and show that a large contribution of the LGM salinity stratification can be explained through lower ocean temperature. In order to extract the maximum information from pore fluid profiles of oxygen isotopes and chloride we evaluate several inverse methods for ill-posed problems and their ability to recover bottom water histories from sediment pore fluid profiles. We demonstrate that Bayesian Markov Chain Monte Carlo parameter estimation techniques enable us to robustly recover the full solution space of bottom water histories, not only at the LGM, but through the most recent deglaciation and the Holocene up to the present. Finally, we evaluate a non-destructive pore fluid sampling technique, Rhizon samplers, in comparison to traditional squeezing methods and show that despite their promise, Rhizons are unlikely to be a good sampling tool for pore fluid measurements of oxygen isotopes and chloride.

Re-estimation of small-scale fishery catches for U.S. flag-associated island areas in the western Pacific: the last 50 years

Nearshore fisheries in the tropical Pacific play an important role, both culturally and as a reliable source of food security, but often remain under-reported in statistics, leading to undervaluation of their importance to communities. We re-estimated nonpelagic catches for Guam and the Commonwealth of the Northern Mariana Islands (CNMI), and summarize previous work for American Samoa for 1950−2002. For all islands combined, catches declined by 77%, contrasting with increasing trends indicated by reported data. For individual island entities, re-estima-tion suggested declines of 86%, 54%, and 79% for Guam, CNMI, and American Samoa, respectively. Except for Guam, reported data primarily represented commercial catches, and hence under-represented contributions by subsistence and recreational fisheries. Guam’s consistent use of creel surveys for data collection resulted in the most reliable reported catches for any of the islands considered. Our re-estimation makes the scale of under-reporting of total catches evident, and provides valuable baselines of likely historic patterns in fisheries catches.

Programa Espacial Brasileiro: militares, cientistas e a questão da soberania nacional

Esta tese versa sobre a análise de um dos grandes projetos tecnológicos do Estado nacional, o PEB, com o intuito de verificar em que medida o Brasil, enquanto País em desenvolvimento e inserido no processo de globalização econômica, tem a possibilidade de autodeterminar um projeto nacional de desenvolvimento relativamente soberano e sustentável, mediante sua capacitação tecnológica em áreas de ponta, como as tecnologias espaciais. Neste ínterim, é discutido o processo de institucionalização da ciência no País e a implantação de um moderno sistema de C&T no Brasil através de uma aliança entre cientistas e militares, culminando com a criação do CNPq em 1951. Apresentamos uma releitura da nossa recente história política e os projetos nacionais de desenvolvimento de que foi alvo o País, formulados pelos grupos sociais mais representativos da sociedade na época estudada, recuperando uma discussão que, estendendo-se por décadas, reservou à questão científica um lugar privilegiado no planejamento do Estado. O período da ditadura militar é especialmente contemplado, considerando-se ter sido esta a fase em que realmente o Programa Espacial Brasileiro sofreu maiores investimentos, conferindo aos militares um papel de destaque no quadro de atores sociais coletivos empenhados no projeto de desenvolvimento do País, destacando as diversas correntes ideológicas em ação dentro das Forças Armadas. Foi analisado o processo de globalização devido ao seu nexo interno e externo com as políticas científicas implantadas ou preconizadas no País. Esse processo, alavancado pela nova dinâmica tecnológica internacional iniciada nos anos 1980, estabeleceu profundos impactos e mudanças na constituição atual da esfera do político. Este é o cenário onde, de nosso ponto de vista, inscreve-se a questão da capacitação científico-tecnológica como variável estratégica em todos os níveis das relações internacionais. A compreensão desta problemática deve ser entendida como parte do cenário mundial que se configurou nas últimas décadas do século XX, tendo no entrelaçamento das dinâmicas científico-tecnológica e a soberania nacional dos Estados uma sinergia diferenciada na reordenação geopolítica contemporânea.

Tropical forest history of the Ecuadorian Andes over the last 34,000 years: preliminary results from pollen and oxygen isotope analyses of Trident 163-13 from the eastern equatorial Pacific [abstract]

EXTRACT (SEE PDF FOR FULL ABSTRACT): Pollen from the upper 2.75 m of a core taken 200 km west of the Golfo de Guayaquil, Ecuador (Trident 163-13, 3° S, 84° W, 3,000 m water depth) documents changes in Andean vegetation and climate of the Cordillera Occidental for ~17,000 years before and after the last glacial maximum.

Trans-Sierran climatic contacts during the last 12,000 years [abstract]

EXTRACT (SEE PDF FOR FULL ABSTRACT): The early-Holocene warm period, ca. 9000 years ago, is a realistic analog for the possible effects of greenhouse warming. At that time the vegetation of the western Sierra Nevada resembled that currently found east of the crest. ... Tourism, water supply, and the logging industry will be negatively effected if climate changes during the next century are in the direction and magnitude of those of the early Holocene. Increased precipitation in the eastern Sierra could offset some of the effects.

ENSO and precipitation variability over Mexico during the last 90 years

Latin America has been shown to be susceptible to climatic anomalies during El Niño/Southern Oscillation (ENSO) events (eg, Aceituno 1988; Ropelewshi and Halpert 1987; Kiladis and Diaz 1989). While these studies have emphasized ENSO-related rainfall and temperature anomalies over Central and South America, less work has been done on the climatic effects of ENSO over the Mexican region. In this study we are investigating interannual and intraseasonal fluctuation in temperature and precipitation over the southwestern United States and Mexico since the turn of the century. We are particularly interested in the effects of ENSO on the interannual variability over this region. This report focuses on the association between ENSO and interannual variability of precipitation over Mexico.

Changes in mid-troposphere snow accumulation on Mt. Logan, Yukon, over the last three centuries

EXTRACT (SEE PDF FOR FULL ABSTRACT): A net snow accumulation time series is presented. It is derived from a 102.5 m ice core retrieved from Mt. Logan at an altitude of 5340 m a.s.l. Annual increments are identified using stable isotopes, trace chemistry, and beta activity. ... The resulting time series of nearly 300 years seems to indicate a lower mean accumulation from AD 1700 to the mid-19th century than after that time. The last 100 years of the series correlates significantly with certain instrumental station records at mid-northern latitudes.