The influence of magnetic field geometry on magnetars X-ray spectra

Nowadays, the analysis of the X-ray spectra of magnetically powered neutron stars or magnetars is one of the most valuable tools to gain insight into the physical processes occurring in their interiors and magnetospheres. In particular, the magnetospheric plasma leaves a strong imprint on the observed X-ray spectrum by means of Compton up-scattering of the thermal radiation coming from the star surface. Motivated by the increased quality of the observational data, much theoretical work has been devoted to develop Monte Carlo (MC) codes that incorporate the effects of resonant Compton scattering (RCS) in the modeling of radiative transfer of photons through the magnetosphere. The two key ingredients in this simulations are the kinetic plasma properties and the magnetic field (MF) configuration. The MF geometry is expected to be complex, but up to now only mathematically simple solutions (self-similar solutions) have been employed. In this work, we discuss the effects of new, more realistic, MF geometries on synthetic spectra. We use new force-free solutions [14] in a previously developed MC code [9] to assess the influence of MF geometry on the emerging spectra. Our main result is that the shape of the final spectrum is mostly sensitive to uncertain parameters of the magnetospheric plasma, but the MF geometry plays an important role on the angle-dependence of the spectra.

Time trials on second-order and variable-learning-rate algorithms

The performance of seven minimization algorithms are compared on five neural network problems. These include a variable-step-size algorithm, conjugate gradient, and several methods with explicit analytic or numerical approximations to the Hessian.

Makrogazdaság-politika és növekedés

A dolgozat röviden áttekinti, hogy az elméleti és empirikus irodalom alapján milyen kapcsolat van a főbb makrogazdasági tényezők (infláció, költségvetési egyenleg) és a gazdasági növekedés között. Ezt követően rátérünk a kelet-közép-európai tapasztalatokra, megvizsgáljuk, hogy a térségben mennyire érvényesülnek az általánosabb eredmények.

Physical oceanography, nutrients, and d18O measured on water bottle samples during POLARSTERN cruise ARK-XXII/2

Extremely low summer sea-ice coverage in the Arctic Ocean in 2007 allowed extensive sampling and a wide quasi-synoptic hydrographic and d18O dataset could be collected in the Eurasian Basin and the Makarov Basin up to the Alpha Ridge and the East Siberian continental margin. With the aim of determining the origin of freshwater in the halocline, fractions of river water and sea-ice meltwater in the upper 150 m were quantified by a combination of salinity and d18O in the Eurasian Basin. Two methods, applying the preformed phosphate concentration (PO*) and the nitrate-to-phosphate ratio (N/P), were compared to further differentiate the marine fraction into Atlantic and Pacific-derived contributions. While PO*-based assessments systematically underestimate the contribution of Pacific-derived waters, N/P-based calculations overestimate Pacific-derived waters within the Transpolar Drift due to denitrification in bottom sediments at the Laptev Sea continental margin. Within the Eurasian Basin a west to east oriented front between net melting and production of sea-ice is observed. Outside the Atlantic regime dominated by net sea-ice melting, a pronounced layer influenced by brines released during sea-ice formation is present at about 30 to 50 m water depth with a maximum over the Lomonosov Ridge. The geographically distinct definition of this maximum demonstrates the rapid release and transport of signals from the shelf regions in discrete pulses within the Transpolar Drift. The ratio of sea-ice derived brine influence and river water is roughly constant within each layer of the Arctic Ocean halocline. The correlation between brine influence and river water reveals two clusters that can be assigned to the two main mechanisms of sea-ice formation within the Arctic Ocean. Over the open ocean or in polynyas at the continental slope where relatively small amounts of river water are found, sea-ice formation results in a linear correlation between brine influence and river water at salinities of about 32 to 34. In coastal polynyas in the shallow regions of the Laptev Sea and southern Kara Sea, sea-ice formation transports river water into the shelf's bottom layer due to the close proximity to the river mouths. This process therefore results in waters that form a second linear correlation between brine influence and river water at salinities of about 30 to 32. Our study indicates which layers of the Arctic Ocean halocline are primarily influenced by sea-ice formation in coastal polynyas and which layers are primarily influenced by sea-ice formation over the open ocean. Accordingly we use the ratio of sea-ice derived brine influence and river water to link the maximum in brine influence within the Transpolar Drift with a pulse of shelf waters from the Laptev Sea that was likely released in summer 2005.

(Table 2) Stable carbon and nitrogen isotope ratios and molar C/N ratio for euchaetid and aetideid copepods during POLARSTERN cruise ANT-XXIII/5

Stable isotope (SI) ratios of carbon (d13C) and nitrogen (d15N) were measured in omnivorous and carnivorous deep-sea copepods of the families Euchaetidae and Aetideidae across the Atlantic sector of the Southern Ocean to establish their trophic positions. Due to high and variable C/N ratios related to differences in lipid content, d13C was corrected using a lipid-normalisation model. d15N signals ranged from 3.0-6.9 per mil in mesopelagic species to 7.0-9.5 per mil in bathypelagic congeners. Among the carnivorous Paraeuchaeta species, the epi- to mesopelagic species Paraeuchaeta antarctica had lower d15N values than the mesopelagic P. rasa and bathypelagic P. barbata. The same trend was observed among omnivorous Aetideidae, but was not significant. In the most abundant species P. antarctica, individuals from the western Atlantic had higher d13C and d15N values than specimens at the eastern stations. These longitudinal changes in d13C and d15N values were attributed to regional differences in hydrography and sea surface temperature (SST), in particular related to a northward extension of the Antarctic Polar Front (APF) at the easternmost stations. The results indicate that even in a mesopelagic carnivorous species, the changes in surface stable isotope signatures are pronounced.

Polonium-210 and Lead-210 activities measured on 17 water bottle profiles and 50 surface water samples during POLARSTERN cruise ARK-XXII/2

Polonium-210 and Lead-210 have been measured in the water column and on suspended particulate matter during the POLARSTERN cruise ARK-XXII/2. The data have been submitted to Pangaea following a Polonium-Lead intercalibration exercise organized by GEOTRACES, where the AWI lab results range within the data standard deviation from 10 participating labs. Polonium-210 and Lead-210 in the ocean can be used to identify the sources and sinks of suspended matter. In seawater, Polonium-210 (210Po) and Lead-210 (210Pb) are produced by stepwise radioactive decay of Uranium-238. 210Po (138 days half life) and 210Pb (22.3 years half life) have high affinities for suspended particles. Those radionuclides are present in dissolved form and adsorbed onto particles. Following adsorption onto particle surfaces, 210Po especially is transported into the interior of cells where it bonds to proteins. In this way, 210Po also accumulates in the food chain. 210Po is therefore considered to be a good tracer for POC, and traces particle export over a timescale of month. 210Pb (22.3 years half life) adsorbs preferably onto structural components of cells, biogenic silica and lithogenic particles, and is therefore a better tracer more rapidly sinking matter. Our goal during ARK XXII/2 was to trace pathways of particulate and dissolved matter leaving the Siberian Shelf. The pathways of particulate and dissolved matter will be followed by the combined use of 210Po and 234Th as a tracer pair (and perhaps 210Pb) for particle flux (Cai, P.; Rutgers van der Loeff, MM (2008) doi:10.1594/PANGAEA.708354). This information gathered from the water column will be complemented with the results of the 210Po-210Pb study in sea ice (Camara-Mor, P, Instituto de Ciencias del Mar-SCIC, Barcelona, Spain) to provide a more thorough picture of particle transport from the shelf to the open sea and from surface to depth.

Integrating SVC and HOL with the PROSPER Toolkit

We describe an integration of the SVC decision procedure with the HOL theorem prover. This integration was achieved using the PROSPER toolkit. The SVC decision procedure operates on rational numbers, an axiomatic theory for which was provided in HOL. The decision procedure also returns counterexamples and a framework has been devised for handling counterexamples in a HOL setting.

Efecto del programa Ruta para la gestión del autocuidado en el control de cifras tensionales en pacientes con hipertensión arterial en una EPS privada de Bogotá, en el año 2015

Introducción. La hipertensión arterial es una de las patologías más representativas en términos de morbi-mortalidad y afectación de la calidad de vida de los usuarios de una EPS privada en Bogotá. Se cuenta en la literatura con múltiples prácticas para favorecer la adherencia al tratamiento de la hipertensión, pero se evidencia que en muchos pacientes no se logran las metas terapéuticas establecidas, generando a largo plazo complicaciones que impactan en la calidad de vida de los pacientes y en el costo en salud. Es por esto que en la EPS se establece desde el 2012 el programa: Ruta para la gestión del autocuidado, como una estrategia de intervención complementaria sobre los pacientes con enfermedades crónicas, con el fin de apoyar a los usuarios del programa de promoción y prevención Atención Específica integral (AEI) en el cumplimiento de las recomendaciones terapéuticas farmacológicas y no farmacológicas generadas por el equipo de salud. La ruta está dirigida especialmente al grupo de pacientes hipertensos con dificultades en la adherencia al programa de promoción y prevención, o en el logro de metas terapéuticas, y busca implementar estrategias de intervención educativa orientadas a fomentar la capacidad de las personas para adaptarse y auto gestionar los desafíos que representa convivir con el diagnóstico de una patología crónica. Por lo anterior la presente investigación busca evaluar el efecto del programa Ruta para la gestión del autocuidado en el control de cifras tensionales en pacientes hipertensos en en una EPS privada de Bogotá en el año 2015. Objetivo. Establecer si la participación en el programa Ruta para la gestión del autocuidado influye en los valores de cifras tensionales de pacientes hipertensos, graduados del programa en una EPS privada de Bogotá en el año 2015. Metodología. Estudio con enfoque cuantitativo, observacional longitudinal retrospectivo de una intervención antes y después, para evaluar el efecto del programa Ruta de gestión de autocuidado, en el control de cifras tensionales, índice de masa corporal y perímetro abdominal de pacientes con diagnóstico de hipertensión arterial afiliados a la EPS privada en Bogotá, graduados del programa entre el 1 de Enero de 2015 a Diciembre de 2015. Población del estudio 409 pacientes, con muestreo por conveniencia. La recolección de datos fue a partir de fuentes secundarias de historia clínica sistematizada de la EPS. Resultados. La población de estudio fueron 409 pacientes, de los cuales el 69,2% son mujeres (n=283). El promedio de la edad de los pacientes fue de 60,16+/-0.9 años, los mayores de 60 años son el grupo más representativo con un 54% (n=220), el estrato socioeconómico 1 es el 77% (n=315), , el tiempo de duración de la ruta de autocuidado de la población analizada más frecuente fue de 4 a 6 meses con un 60,4% (n=247) y el tratamiento más utilizado es el combinado con 53,1% (n=217). Antes del inicio de la Ruta de gestión de autocuidado, 138 pacientes tuvieron valores de tensión arterial sistólica en rangos de hipertensión, al finalizar la misma disminuyeron los valores a rangos de normalidad 96 pacientes (69,6%). De los pacientes que iniciaron con tensión arterial sistólica en rangos de normalidad (n=271), el 12,5% al finalizar la ruta tuvieron valores en rangos de hipertensión (n=34). El cambio en los rangos de tensión arterial sistólica evidenció que es estadísticamente significativo (p=0.000) con un OR de 2,8:1, lo cual indica que la variación de pacientes con valores de tensión arterial sistólica en rangos de hipertensión a valores en rango de normotensión, ocurre 2,8 veces más en quienes realizan la ruta de gestión de autocuidado que los que no. Antes del inicio de la Ruta de gestión de autocuidado, 70 pacientes tuvieron valores de tensión arterial diastólica en rangos de hipertensión, al finalizar la misma disminuyeron los valores a rangos de normalidad 56 pacientes (80%). De los pacientes que iniciaron con tensión arterial diastólica en rangos de normalidad (n=339), el 8,3% al finalizar la ruta tuvieron valores en rangos de hipertensión (n=28). El cambio en los rangos de tensión arterial diastólica, evidenció que es estadísticamente significativo (p=0.001) con un OR de 2,0:1, lo cual indica que la variación de pacientes con valores de tensión arterial diastólica en rangos de hipertensión a valores en rango de normotensión, ocurre 2 veces más en quienes realizan la ruta de gestión de autocuidado que los que no. Conclusión. La implementación de modelos educativos en la atención primaria en salud en las unidades de atención de servicios ambulatorios en la EPS, generan un impacto positivo en el control de las cifras tensionales. El tener pacientes controlados incide en la disminución de morbimortalidad, costos de hospitalización médica y mejora en la calidad de vida.

Na 1 Nachlass Max Horkheimer, 622 - Unterlagen zu einführenden Vorlesungen (p. VIII 41,1-2-VIII 41b)

"Problem der neueren Philosophie", Vorlesung Wintersemester 1950/51 und Sommersemester 1951, 1) Heft, 78 Blatt und 20 zusätzliche Blätter, eigenhändige Notizen (GS 14, S. 145, 151-152), 2) Friedrich Pollock: Notizen zur Volesung Max Horkheimers, Wintersemester 1950/51), eigenhändige Notizen, 9 Blatt; "Philosophie im 17. Jahrhundert (insbes. Spinoza)", Vorlesung Winteremester 1951/52, 1) Heft 1, 17 Blatt und 2 zusätzliche Blätter, eigenhändige Notizen, 2) Heft 2, 46 Blatt, davon 3 leer, und 15 zusätzliche Blätter, eigenhändige Notizen; "Philosophie im 18. Jahrhundert", Vorlesung Sommersemester 1952, 1 Heft mit eigenhändigen Notizen, 64 Blatt, davon 30 leer, und 44 zusätzliche Blätter;

Contiunous surface water uncorrected and quench-corrected active fluorescence and derived chlorophyll a concentration using calibration by HPLC pigments during POLARSTERN cruise ANT-XXV/1

The relationship between phytoplankton assemblages and the associated optical properties of the water body is important for the further development of algorithms for large-scale remote sensing of phytoplankton biomass and the identification of phytoplankton functional types (PFTs), which are often representative for different biogeochemical export scenarios. Optical in-situ measurements aid in the identification of phytoplankton groups with differing pigment compositions and are widely used to validate remote sensing data. In this study we present results from an interdisciplinary cruise aboard the RV Polarstern along a north-to-south transect in the eastern Atlantic Ocean in November 2008. Phytoplankton community composition was identified using a broad set of in-situ measurements. Water samples from the surface and the depth of maximum chlorophyll concentration were analyzed by high performance liquid chromatography (HPLC), flow cytometry, spectrophotometry and microscopy. Simultaneously, the above- and underwater light field was measured by a set of high spectral resolution (hyperspectral) radiometers. An unsupervised cluster algorithm applied to the measured parameters allowed us to define bio-optical provinces, which we compared to ecological provinces proposed elsewhere in the literature. As could be expected, picophytoplankton was responsible for most of the variability of PFTs in the eastern Atlantic Ocean. Our bio-optical clusters agreed well with established provinces and thus can be used to classify areas of similar biogeography. This method has the potential to become an automated approach where satellite data could be used to identify shifting boundaries of established ecological provinces or to track exceptions from the rule to improve our understanding of the biogeochemical cycles in the ocean.