North Pacific Carbon Cycle Response to Climate Variability on Seasonal to Decadal Timescales

Climate variability drives significant changes in the physical state of the North Pacific, and there may be important impacts of this variability on the upper ocean carbon balance across the basin. We address this issue by considering the response of seven biogeochemical ocean models to climate variability in the North Pacific. The models' upper ocean pCO(2) and air-sea CO(2) flux respond similarly to climate variability on seasonal to decadal timescales. Modeled seasonal cycles of pCO(2) and its temperature- and non-temperature-driven components at three contrasting oceanographic sites capture the basic features found in observations (Takahashi et al., 2002, 2006; Keeling et al., 2004; Brix et al., 2004). However, particularly in the Western Subarctic Gyre, the models have difficulty representing the temporal structure of the total pCO(2) seasonal cycle because it results from the difference of these two large and opposing components. In all but one model, the air-sea CO(2) flux interannual variability (1 sigma) in the North Pacific is smaller ( ranges across models from 0.03 to 0.11 PgC/yr) than in the Tropical Pacific ( ranges across models from 0.08 to 0.19 PgC/yr), and the time series of the first or second EOF of the air-sea CO(2) flux has a significant correlation with the Pacific Decadal Oscillation (PDO). Though air-sea CO(2) flux anomalies are correlated with the PDO, their magnitudes are small ( up to +/- 0.025 PgC/yr ( 1 sigma)). Flux anomalies are damped because anomalies in the key drivers of pCO(2) ( temperature, dissolved inorganic carbon (DIC), and alkalinity) are all of similar magnitude and have strongly opposing effects that damp total pCO(2) anomalies.

Poetica Hebraica harmonica, rhythmica, metrica, praeceptis, commentariis, regulis, exemplis perspicue declarata

Vorlage d. Digitalisats aus d. Besitz d. Theol. Hochschule St. Georgen

Should Texas use public funding for bariatric surgery?

Background. Obesity in America has increased exponentially since the 1970s with no sign of slowing down. It is a major public health problem, and is currently the second leading cause of preventable deaths in America (Flegal et al., 2010). Bariatric surgery is currently the only approved therapy that has shown to have a lasting impact on obese patients. While the initial cost of the surgery remains high, numerous cost-benefit analyses have demonstrated an overall cost saving within two to five years (McEwen et al., 2010). Only three states, including Texas, do not currently fund bariatric surgery through Medicare and Medicaid. ^ Objectives. To determine whether the current data on the cost-benefit analysis of bariatric surgery supports Texas' decision to not publicly fund bariatric surgery through its Medicare and Medicaid programs. ^ Methods. We conducted literature reviews to determine the current cost of obesity in Texas as well as the methods being employed to treat obesity currently. We then analyzed the history of bariatric surgery and its current implementation, looking at safety and the future benefits of bariatric surgery. We then looked at key cost-benefit analyses and meta-analyses to determine the cost effectiveness of bariatric surgery. We then analyzed both direct medical expenditures and indirect benefits of bariatric surgery. ^ Conclusions. If the obesity epidemic continues unabated, it will become one of the leading health expenditures in Texas within decades. Given that surgery is currently the only approved therapy for obesity that has been shown to be effective in the majority of patients, Texas' decision not to publicly fund bariatric surgery is short sighted.^

(Table 2) Chemical composition of quenched glasses from the Mohns and Knipovich Ridges

The aim of this project was a petrogeochemical study of igneous rocks in the areas of the Mohns and Knipovich Ridges, both being the northern extensions of the Mid-Atlantic Ridge (MAR), using data available for quenching glass samples collected during Cruises 36 and 38 of R/V Akademic Mstislav Keldysh and during Cruise 15 of R/V Professor Logachev. Results of igneous rock studying from the Mohns and Knipovich Ridges at the background of evolution of the total North Atlantic Province, which had been identified earlier from tectonic and geophysical data, showed that igneous rocks of the Knipovich Ridge can be ranked as shallow tholeiites, primary melts of which were relatively rich in Na and Si and poor in Fe. This type of magma is characteristic of colder regions of the oceanic lithosphere. Its occurrence in the Knipovich Ridge and its potential propagation up to the Gakkel Ridge suggest that igneous rocks of this region originated under conditions of passive spreading in contrast to the MAR region in vicinity of Iceland and Azores, where substantial contribution of hotter material of a rising plume contributed to formation of the oceanic crust. The North Atlantic Ocean is the youngest province in terms of ocean-floor opening. Geologically and geophysically it is one of well studied regions of the World Ocean. Nevertheless some basic key items of its origin still remain to be clarified. In 1975 Scatler et al. proved specifics of this region manifested in growth of the gravity field, and also in relative height of the ocean floor in the region of 33-70°N, which was associated by them with rise of the hotter mantle, as compared with common regions of the Mid-Atlantic Ridge. Later this view was confirmed by character of magmatism, which differed in depth of generation and by melting degree of the resulting primary magma. Uniqueness of the North Atlantic region was also proved by the fact that this region was marked by extensive geochemical anomalies associated with Azores, Iceland, and Jan Mayen. All of these data allow to consider the northern part of the MAR (north of 33°N) as an united global geotectonic province. The Mohns and Knipovich Ridges located north of Iceland locate at the northern end of this province. This is the least known region. Therefore, new data for ridge areas of 73-77°N are needed for more complete geologic history of the Arctic Basin. The aim of this study was to carry out a complex comparison of magmatism at the Mohns and Knipovich Ridges with magmatism at large segments of the MAR northern province and to reconstruct mechanisms of primary magma formation, as well as conditions of their fractionation. This paper was based on results of studying quenched glasses, which reflect evolution of melt in the course of its formation.

Las estrategias en el lugar de trabajo del Partido Comunista en Argentina desde sus orígenes hasta 1943 : Células, comités de fábricas y comisiones internas

La intención de nuestro trabajo es recuperar la experiencia impulsada por el Partido Comunista (PC) a partir de su creación y hasta la irrupción del peronismo en la organización del movimiento obrero en los sitios de producción. Durante años la creencia extendida en la historiografía asociaba la militancia en los espacios de base con el modelo sindical peronista y la instalación de las comisiones internas. Recientes investigaciones demostraron el extenso entramado organizacional de base generado por el proletariado fabril en las décadas anteriores a 1943. En dicho proceso coadyuvaron las corrientes de izquierda y en particular el PC que enarboló una política específica para su inserción en las fábricas y empresas. Los ejes que guían nuestra pesquisa son variados: las formas que adquirió esta militancia de base, el impacto de las líneas estratégicas partidarias, entre otros.

Inmigración y trabajo irregular en la agricultura: trabajadores tamaulipecos en Estados Unidos y jornaleros magrebíes en Andalucía

Tanto en Estados Unidos como en España, la escasez de mano de obra local dispuesta a aceptar las condiciones sociolaborales imperantes en la agricultura, unida a la dificultad de inspeccionar y regular un sector donde la movilidad de trabajadores es constante, ha conducido a que la agricultura sea la actividad donde encuentran empleo más fácilmente los trabajadores migrantes indocumentados. En Estados Unidos la demanda de empleo en la agricultura ha venido siendo cubierta principalmente por trabajadores mexicanos; mientras, en España, los jornaleros procedentes de Marruecos constituyen el colectivo de inmigrantes con mayor presencia en el sector agrario. Este artículo, fundamentado en una metodología cualitativa, analiza, por una parte, la situación socio-laboral de los inmigrantes procedentes de Marruecos en la agricultura de Andalucía, región situada en el sur de España. Por otra parte, examina la situación de los jornaleros de Tamaulipas, región situada en el noreste de México, empleados de forma estacional en el sector agrario estadounidense

Project development for older adults : Orientation's contribution

This paper systematizes the work developed during the first year of the initiation scholarship for the research project entitled 'Orientation within the new Active Aging Model: educational, work-related, personal and social choices (1)'. This project articulates the Active Aging Model and the Theoretical Operative Model in Orientation, in order to learn how new projects are developed by older adults who used to be part of the formal system of labor and by those who were out of it, and to design programmatic proposals for educational, work-related, personal and social Orientation choices for such population. The sample is made up by seventy people between 64 and 74 years of age, residing in La Plata. The first conclusions evidence the importance that older adults place on project development at this stage of their life cycle, giving special importance to educational, personal and social projects; as well as on the identification of economic factors, health state, family needs for care and social support, among other things, as conditioning the fulfillment of such projects. The differences found in terms of the labor system they used to belong to can be especially observed in the type of project developed.

Elaboración de proyectos en adultos mayoresz : Aportes de la orientación

El presente trabajo sistematiza la labor desarrollada durante el primer año de la beca de iniciación del proyecto de investigación 'La Orientación en el nuevo modelo de envejecimiento activo: elecciones educativas, laborales, personales, sociales (1)'. Dicho proyecto articula el Modelo de Envejecimiento Activo y el Modelo Teórico Operativo en Orientación, con el propósito de conocer cómo elaboran los nuevos proyectos los adultos mayores que pertenecieron al sistema formal de trabajo y aquellos que permanecieron fuera de él, y diseñar propuestas programáticas de Orientación y elección educativa, laboral, personal y social destinadas a esta población. La muestra está conformada por sesenta personas de entre 64 y 74 años de edad, residentes en la Ciudad de La Plata. Las primeras conclusiones dan cuenta de la importancia que atribuyen los adultos mayores a la elaboración de proyectos en esta etapa del ciclo vital, prevaleciendo los proyectos educativos, personales y sociales; así como la identificación de factores económicos, condiciones de salud, demanda de cuidados de otros familiares y apoyo social, entre otros, como condicionantes para la concreción de dichos proyectos. Las diferencias encontradas con respecto al sistema de trabajo al que han pertenecido se observan principalmente en el tipo de proyecto elaborado

Benthic oxygen flixes on the Washington shelf and slope

Benthic oxygen fluxes calculated from in situ microelectrode profiles arc compared with benthic flux chamber O2 uptake measurements on a transect of eight stations across the continental shelf and three stations on the slope of Washington State. Station depths ranged from 40 to 630 m and bottom-water oxygen concentrations were 127-38 µM. The fluxes measured by the two methods were similar on the slope, but on the shelf, the chamber flux exceeded the microelectrode flux by as much as a factor of 3-4. We attribute this difference to pore-water irrigation, a process which apparently accounts for the oxidation of a significant amount of organic C in the continental shelf sediments. Combining our diffusive flux data with other data demonstrates clearly that the bottomwater oxygen concentration must play some significant role in determining the sedimentary oxygen consumption rate. Numerical simulation of the microelectrode 0, profiles suggests that roughly half the diffusive 0, flux must be consumed within - 1 mm of the sediment surface. If this conclusion is correct, then the magnitude of the diffusive flux depends both on the bottom-water oxygen concentration and on the supply rate of labile C to the sediment surf'ace.