986 resultados para Duanes-Regulació-València-1670


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Reinhard Voskens. Schrifft Schneider und Giesser wohnhaft in der Lauten gasse. in der Korn-Blum. zu Franckfurt am Main

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Bibliogr. Nachweis: Uit het Leidse Prentenkabinet : over tekeningen, prenten en fotos / Schaeps, Jef [Hrsg.]. - Leiden : Primavera, 2001. - S. 85-87); Hollstein 2

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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.

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For the first time deep-sea mooring stations with sediment traps were deployed in the northeast Black Sea. One sediment trap for long-term studies was located at Station 1 (44°15'N, 37°43'E, deployment depth 1800 m, depth 1900 m). The trap collected sinking sedimentary material from January to May 1998. Material collectors were changed every 15 days. Other stations with sediment traps for short-term studies (September-October 1999) were located on the shelf: Station 2 (44°16'N, 38°37'E, deployment depth 45 m, depth 50 m) and on the bottom of the canyon: Station 3 (44°16'N, 38°22'E, deployment depth 1145 m, depth 1150 m), Station 4 (44°11'N, 38°21'E, deployment depths 200, 1550, 1650 m, depth 1670 m). Collected material indicates that vertical particle fluxes are controlled by seasonal changes of in situ production and by dynamics of terrigenous matter input. Higher vertical particle flux of carbonate and biogenic silica was in spring due to bloom of plankton organisms. Maximum of coccolith bloom is in April-May. Bloom of diatoms begins in March. In winter and autumn lithogenic material dominates in total flux. Its amount strongly depends on storms and river run-off. Suspended particle material differs from surface shelf sediments by finer particles (mainly clay fraction) and high content of clay minerals and biogenic silica. This material may form lateral fluxes with higher concentration of particles transported along the bottom of deep-sea canyons from the shelf to the deep basin within the nepheloid layer. In winter such transportation of sedimentary material is more intensive due to active vertical circulation of water masses.

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El propósito general de nuestro trabajo es ofrecer un análisis del lugar que ocupó la voluntad divina en el corpus leibniziano. Lo voluminoso de la obra de Leibniz, sus dificultades de datación, la virtud grafómana de nuestro filósofo y el modo apretado en que trabó un concepto con otro, han llevado a una gran dispersión interpretativa que, por lo general, no se ha detenido a analizar de manera lo suficientemente "autónoma" el rol preponderante que Leibniz fue otorgando a esa facultad. La prevalencia de las "interpretaciones intelectualistas" en la literatura secundaria tiende a desdibujar el protagonismo que sucesivamente adquiriría la voluntad divina en el plan de una fundamentación de la teodicea leibniziana. La conciliación de los atributos de Dios con la existencia del mal en el mundo surgió tempranamente de la necesidad de combatir el sofisma que responsabiliza a Dios por las faltas y sufrimientos humanos. La voluntad estuvo en el centro de la cuestión desde los primeros años de la década de 1670. No obstante, el fuerte intelectualismo de esta primera época parece haber sellado las claves de un cuasi monopolio interpretativo que arroja a la voluntad al lugar segundón que le deja el entendimiento

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El propósito general de nuestro trabajo es ofrecer un análisis del lugar que ocupó la voluntad divina en el corpus leibniziano. Lo voluminoso de la obra de Leibniz, sus dificultades de datación, la virtud grafómana de nuestro filósofo y el modo apretado en que trabó un concepto con otro, han llevado a una gran dispersión interpretativa que, por lo general, no se ha detenido a analizar de manera lo suficientemente "autónoma" el rol preponderante que Leibniz fue otorgando a esa facultad. La prevalencia de las "interpretaciones intelectualistas" en la literatura secundaria tiende a desdibujar el protagonismo que sucesivamente adquiriría la voluntad divina en el plan de una fundamentación de la teodicea leibniziana. La conciliación de los atributos de Dios con la existencia del mal en el mundo surgió tempranamente de la necesidad de combatir el sofisma que responsabiliza a Dios por las faltas y sufrimientos humanos. La voluntad estuvo en el centro de la cuestión desde los primeros años de la década de 1670. No obstante, el fuerte intelectualismo de esta primera época parece haber sellado las claves de un cuasi monopolio interpretativo que arroja a la voluntad al lugar segundón que le deja el entendimiento