La epidemiología crítica: una nueva forma de mirar la salud en el espacio urbano

La epidemiología empírico-analítica asume como un pilar interpretativo la noción de "lugar" para las descripciones que construye. La epidemiología crítica supera esa noción restrictiva y propone una construcción innovadora del espacio de la salud urbana retomando los aportes de la teoría crítica del espacio y la geografía, y articulando estos avances con los de la propia epidemiología desde una perspectiva de la determinación social de la salud. Desde esta óptica se repiensa la relación urbano-rural a la luz de los procesos históricos de aceleración, drástica pérdida de sustentabilidad y profunda inequidad urbanas, así como del papel de la nueva ruralidad capitalista monopólica, en avivar el cierre del espacio de la vida en nuestras ciudades. Se busca superar el mito de la dualidad urbano rural, se cuestiona el paradigma dominante de la modernidad que impuso la comprensión de dos mundos prácticamente contrapuestos: la ciudad como rectora, cosmopolita, avanzada y pujante, y lo rural como un mundo atrasado, local, más simple, y secundario, pues en años más recientes, la distinción clásica entre lo urbano y lo rural se hace cada vez más difícil, lamentablemente con una perversa dialéctica de deterioro e influjos malsanos de uno a otro espacio.

A groove-ploughing theory for the production of mega-scale glacial lineations, and implications for ice-stream mechanics

Mega-scale glacial lineations (MSGLs) are longitudinally aligned corrugations (ridge-groove structures 6-100 km long) in sediment produced subglacially. They are indicators of fast flow and a common signature of ice-stream beds. We develop a qualitative theory that accounts for their formation, and use numerical modelling, and observations of ice-stream beds to provide supporting evidence. Ice in contact with a rough (scale of 10-10(3) m) bedrock surface will mimic the form of the bed. Because of flow acceleration and convergence in ice-stream onset zones, the ice-base roughness elements experience transverse strain, transforming them from irregular bumps into longitudinally aligned keels of ice protruding downwards. Where such keels slide across a soft sedimentary bed, they plough through the sediments, carving elongate grooves, and deforming material up into intervening ridges. This explains MSGLs and has important implications for ice-stream mechanics. Groove ploughing provides the means to acquire new lubricating sediment and to transport large volumes of it downstream. Keels may provide basal drag in the force budget of ice streams, thereby playing a role in flow regulation and stability We speculate that groove ploughing permits significant ice-stream widening, thus facilitating high-magnitude ice discharge.

Onset of recent rapid sea-level rise in the western Atlantic Ocean

A high-resolution record of sea-level change spanning the past 1000 years is derived from foraminiferal and chronological analyses of a 2m thick salt-marsh peat sequence at Chezzetcook, Nova Scotia, Canada. Former mean tide level positions are reconstructed with a precision of +/- 0.055 in using a transfer function derived from distributions of modern salt-marsh foraminifera. Our age model for the core section older than 300 years is based on 19 AMS C-14 ages and takes into account the individual probability distributions of calibrated radiocarbon ages. The past 300 years is dated by pollen and the isotopes Pb-206, Pb-207, Pb-210, Cs-137 and Am-241. Between AD 1000 and AD 1800, relative sea level rose at a mean rate of 17cm per century. Apparent pre-industrial rises of sea level dated at AD 1500-1550 and AD 1700-1800 cannot be clearly distinguished when radiocarbon age errors are taken into account. Furthermore, they may be an artefact of fluctuations in atmospheric C-14 production. In the 19th century sea level rose at a mean rate of 1.6mm/yr. Between AD 1900 and AD 1920, sea-level rise accelerated to the modern mean rate of 3.2mm/yr. This acceleration corresponds in time with global temperature rise and may therefore be associated with recent global warming. (c) 2005 Elsevier Ltd. All rights reserved.