983 resultados para Stanhope, Walter Spencer, 1749-1822.
Resumo:
Fil: Torchia Estrada, Juan Carlos.
Resumo:
Fil: González de Díaz Araujo, Graciela. Universidad Nacional de Cuyo. Facultad de Artes y Diseño
Resumo:
Fil: Fontana, Esteban.
Resumo:
Fil: Ares, Consuelo.
Resumo:
Este artigo apresenta algumas das principais linhas do projeto de pesquisa «Scholastica colonialis», que tem o objetivo de investigar de forma exaustiva o desenvolvimento da filosofia escolástica barroca na América Latina, durante parte significativa do período colonial, isto é, séculos 16-18. Até hoje, a principal proposta de pesquisa sobre os materiais existentes e os méritos da filosofia «colonial» e «barroca» foi aquela exemplificada pelos estudos de Walter B. Redmond. Assim, busca-se expor, resumidamente, o status quaestionis que a síntese de seus trabalhos permite concluir.
Resumo:
Fil: Fernández Robbio, Matías Sebastián. Universidad Nacional de Cuyo
Resumo:
En este artículo tenemos como objetivo mostrar que, por una parte, en oposición a la teoría de William of Ockham, las teorías de Walter Chatton y Adam of Wodeham convienen con la doctrina contemporánea según la cual los estados mentales son estados funcionales de un cierto tipo. Por otra parte, en este artículo queremos revelar que aquellas teorías medievales que podemos llamar funcionalistas fundamentan una perspectiva económica medieval respecto a la composición de un ser humano.
Resumo:
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.
Resumo:
We rediscovered a temperature time series from Heinrich W. M. Olbers. Heinrich W. M. Olbers measured in Bremen, Sandstrasse 15, in Germany from 1803 to 1821 three times a day (7 am, 1-2 pm and 10 pm) the temperature at his window of his study, which is up to 16 m above the zero marking at the Weserbrücke. The temperature values from 1814 are missing. We got the temperature values from different sources in the Olbers estate. We calculated the daily mean and digitized it in various plots. A very small trend towards cooling is apparent in the data which might be insignificant. But a clear seasonal trend was identifiable: the late winter and the early spring were becoming warmer, while the summer and early autumn became cooler. The average temperature in Bremen was 8.3606 deg C at that time. Additionally we combined the newly discovered Heinrich W. M. Olbers temperature data and the Heinemann and Bätjer data to see whether there are great differences between these two time series. Although the temperatures of Heinrich W. M. Olbers are in general cooler than the Heinemann and Bätjer data they fit together.
Resumo:
Fil: Bonilla, Manuel. Universidad Nacional de La Plata. Facultad de Humanidades y Ciencias de la Educación; Argentina.