863 resultados para Danish poetry.


Relevância:

20.00% 20.00%

Publicador:

Resumo:

Fil: Errecalde, Alejandro Martín. Universidad Nacional de La Plata. Facultad de Humanidades y Ciencias de la Educación; Argentina.

Relevância:

20.00% 20.00%

Publicador:

Resumo:

Fil: Zecchin de Fasano, Graciela Cristina. Universidad Nacional de La Plata. Facultad de Humanidades y Ciencias de la Educación; Argentina.

Relevância:

20.00% 20.00%

Publicador:

Resumo:

La traducción se planta como el medio para que un público ajeno a la lengua de origen de un texto pueda acceder a él. En el caso de la poesía, debido a su difícil traducción y a su escasa publicación, la problemática de la traducción se torna doble. A partir de entonces, la presentación de una antología poética argentina en inglés como carta de presentación de la literatura nacional en el mundo resulta una obra interesante en cuanto a sus contenidos y repercusiones en el canon internacional

Relevância:

20.00% 20.00%

Publicador:

Resumo:

La traducción se planta como el medio para que un público ajeno a la lengua de origen de un texto pueda acceder a él. En el caso de la poesía, debido a su difícil traducción y a su escasa publicación, la problemática de la traducción se torna doble. A partir de entonces, la presentación de una antología poética argentina en inglés como carta de presentación de la literatura nacional en el mundo resulta una obra interesante en cuanto a sus contenidos y repercusiones en el canon internacional

Relevância:

20.00% 20.00%

Publicador:

Resumo:

Fil: Errecalde, Alejandro Martín. Universidad Nacional de La Plata. Facultad de Humanidades y Ciencias de la Educación; Argentina.

Relevância:

20.00% 20.00%

Publicador:

Resumo:

1. Winter temperatures differ markedly on the Canadian prairies compared with Denmark. Between 1 January 1998 and 31 December 2002, average weekly and monthly temperatures did not drop below 0 °C in the vicinity of Silkeborg, Denmark. Over this same time, weekly average temperatures near Calgary, Alberta, Canada, often dropped below -10 °C for 3-5 weeks and the average monthly temperature was below 0 °C for 2-4 months. Accordingly, winter ice conditions in shallow lakes in Canada and Denmark differed considerably. 2. To assess the implications of winter climate for lake biotic structure and function we compared a number of variables that describe the chemistry and biology of shallow Canadian and Danish lakes that had been chosen to have similar morphometries. 3. The Danish lakes had a fourfold higher ratio of chlorophyll-a: total phosphorus (TP). Zooplankton : phytoplankton carbon was related to TP and fish abundance in Danish lakes but not in Canadian lakes. There was no significant difference in the ratio log total zooplankton biomass : log TP and the Canadian lakes had a significantly higher proportion of cladocerans that were Daphnia. These differences correspond well with the fact that the Danish lakes have more abundant and diverse fish communities than the Canadian lakes. 4. Our results suggest that severe Canadian winters lead to anoxia under ice and more depauperate fish communities, and stronger zooplankton control on phytoplankton in shallow prairie lakes compared with shallow Danish lakes. If climate change leads to warmer winters and a shorter duration of ice cover, we predict that shallow Canadian prairie lakes will experience increased survivorship of planktivores and stronger control of zooplankton. This, in turn, might decrease zooplankton control on phytoplankton, leading to 'greener' lakes on the Canadian prairies.

Relevância:

20.00% 20.00%

Publicador:

Resumo:

Continuous Wavelet Transform was applied to bed elevation profiles (BEP) and used in the study in order to recognise the spatial distribution of bedforms and discriminate between their hierarchical scales. In particular, the spatial distribution of the hierarchical scales is highlighted by averaging wavelet power spectra over different bands, and displayed as the wavelet variance of the BEP (see map). Four dune classes were defined, following Ashley (1990): small dunes (1-5 m), medium dunes (5-10 m), large dunes (10-100 m), and very large dunes (>100 m).