921 resultados para Vancouver 2010 Olympic Winter Games


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Observations of the ozone profile by a ground-based microwave radiometer in Switzerland indicate a dominant 20-day oscillation in stratospheric ozone, possibly related to oscillations of the polar vortex edge during winter. For further understanding of the nature of the 20-day oscillation, the ozone data set of ERA Interim meteorological reanalysis is analyzed at the latitude belt of 47.5° N and in the time from 1979 to 2010. Spectral analysis of ozone time series at 7 hPa indicates that the 20-day oscillation is maximal at two locations: 7.5° E, 47.5° N and 60° E, 47.5° N. Composites of the stream function are derived for different phases of the 20-day oscillation of stratospheric ozone at 7 hPa in the Northern Hemisphere. The streamline at Ψ = −2 × 107 m2 s−1 is in the vicinity of the polar vortex edge. The other streamline at Ψ = 4 × 107 m2 s1 surrounds the Aleutian anticyclone and goes to the subtropics. The composites show 20-day period standing oscillations at the polar vortex edge and in the subtropics above Northern Africa, India, and China. The 20-day period standing oscillation above Aral Sea and India is correlated to the strength of the Aleutian anticyclone.

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Thawing-induced cliff top retreat in permafrost landscapes is mainly due to thermo-erosion. Ground-ice-rich permafrost landscapes are specifically vulnerable to thermo-erosion and may show high degradation rates. Within the HGF Alliance Remote Sensing and the FP7 PAGE21 permafrost programs we investigated how SAR and optical remote sensing can contribute to the monitoring of erosion rates of ice-rich cliffs in Arctic Siberia (Lena Delta, Russia). We produced two different vector products: i) Intra-annual cliff top retreat based on TerraSAR-X (TSX) satellite data (2012-2014): High-temporal resolution time series of TSX satellite data allow the inter-annual and intra-annual monitoring of the upper cliff-line retreat also under bad weather conditions and continuous cloud coverage. This published SAR product contains the retreating upper cliff lines of a 1.5 km long part of eroding ice-rich coast of Kurungnakh Island in the central Lena Delta. The upper cliff line was mapped using a thresholding approach for images acquired in the years 2012, 2013 and 2014 for the months June (2013, 2014), July (2013, 2014), August (2012, 2013, 2014) and September (2013, 2014). The cliff top retreat vector product is called 'upper_cliff_TerraSAR-X'. While the 2014 cliff lines show a clear retreat of 2 to 3 m/month, the cliff top lines for 2012 and 2013 are not chronologically ordered. However, lines from the end of the season of a year are always close to the lines from the beginning of the next summer season, indicating low cliff retreat in winter. ii) 4-year cliff top retreat based on optical satellite data (2010-2014): Long-term cliff top retreat could be assessed with two high-spatial resolution optical satellite images (GeoEye-1, 2010-08-05 and Worldview-1, 2014-08-19). The cliff top retreat vector product is called 'upper_cliff_optical'. Results: The long-term cliff top retreat derived from optical satellite data are 35 m cliff retreat within 4 years. The higher-temporal resolution SAR data equivalently show long-term rates of 18 m within 2 years and nearly now degradation activities in winter but maximum erosion rates in summer months.The Intra-seasonal cliff top retreat lines from 2014 show a rate of 2 to 3 m per month.

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We conducted a six-week investigation of the sea ice inorganic carbon system during the winter-spring transition in the Canadian Arctic Archipelago. Samples for the determination of sea ice geochemistry were collected in conjunction with physical and biological parameters as part of the 2010 Arctic-ICE (Arctic - Ice-Covered Ecosystem in a Rapidly Changing Environment) program, a sea ice-based process study in Resolute Passage, Nunavut. The goal of Arctic-ICE was to determine the physical-biological processes controlling the timing of primary production in Arctic landfast sea ice and to better understand the influence of these processes on the drawdown and release of climatically active gases. The field study was conducted from 1 May to 21 June, 2010.

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Se analiza la lucha fratricida entre Pedro I y Enrique II de Castilla a la luz del "Cuento de los Reyes" inserto en El Victorial, de Gutierre Díaz de Games, y de las Crónicas de Pero López de Ayala. En el transcurso de una guerra civil, inscripta en un conflicto aún mayor, la Guerra de los Cien Años, dos reyes luchan por la misma corona. Ya que Pedro I tiene un origen claramente legítimo, los cronistas, favorables al usurpador Enrique, deben crear para éste una legitimidad, basada en este caso en la denuncia del profundo daño que causa al reino la notoria inconducta del rey legítimo. Una vez perpetrado el doble crimen que significa el asesinato de Pedro a manos de Enrique ?a la vez fratricidio y regicidio? se ejerce la violencia en su función fundacional, instaurando a la vez un nuevo reinado y una nueva dinastía. Por otra parte, lo que sucede en la cúspide de la sociedad se repite en otros niveles, ya que en la guerra civil también se cometerían fratricidios, porque el enemigo no es el Otro, sino un Igual.

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Se analiza la lucha fratricida entre Pedro I y Enrique II de Castilla a la luz del "Cuento de los Reyes" inserto en El Victorial, de Gutierre Díaz de Games, y de las Crónicas de Pero López de Ayala. En el transcurso de una guerra civil, inscripta en un conflicto aún mayor, la Guerra de los Cien Años, dos reyes luchan por la misma corona. Ya que Pedro I tiene un origen claramente legítimo, los cronistas, favorables al usurpador Enrique, deben crear para éste una legitimidad, basada en este caso en la denuncia del profundo daño que causa al reino la notoria inconducta del rey legítimo. Una vez perpetrado el doble crimen que significa el asesinato de Pedro a manos de Enrique ?a la vez fratricidio y regicidio? se ejerce la violencia en su función fundacional, instaurando a la vez un nuevo reinado y una nueva dinastía. Por otra parte, lo que sucede en la cúspide de la sociedad se repite en otros niveles, ya que en la guerra civil también se cometerían fratricidios, porque el enemigo no es el Otro, sino un Igual.

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Se analiza la lucha fratricida entre Pedro I y Enrique II de Castilla a la luz del "Cuento de los Reyes" inserto en El Victorial, de Gutierre Díaz de Games, y de las Crónicas de Pero López de Ayala. En el transcurso de una guerra civil, inscripta en un conflicto aún mayor, la Guerra de los Cien Años, dos reyes luchan por la misma corona. Ya que Pedro I tiene un origen claramente legítimo, los cronistas, favorables al usurpador Enrique, deben crear para éste una legitimidad, basada en este caso en la denuncia del profundo daño que causa al reino la notoria inconducta del rey legítimo. Una vez perpetrado el doble crimen que significa el asesinato de Pedro a manos de Enrique ?a la vez fratricidio y regicidio? se ejerce la violencia en su función fundacional, instaurando a la vez un nuevo reinado y una nueva dinastía. Por otra parte, lo que sucede en la cúspide de la sociedad se repite en otros niveles, ya que en la guerra civil también se cometerían fratricidios, porque el enemigo no es el Otro, sino un Igual.

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The marine laboratories in Plymouth have sampled at two principle sites in the Western English Channel for over a century in open-shelf (station E1; 50° 02'N, 4° 22'W) and coastal (station L4; 50° 15'N, 4° 13'W) waters. These stations are seasonally stratified from late-April until September, and the variable biological response is regulated by subtle variations in temperature, light, nutrients and meteorology. Station L4 is characterized by summer nutrient depletion, although intense summer precipitation, increasing riverine input to the system, results in pulses of increased nitrate concentration and surface freshening. The winter nutrient concentrations at E1 are consistent with an open-shelf site. Both stations have a spring and autumn phytoplankton bloom; at station E1, the autumn bloom tends to dominate in terms of chlorophyll concentration. The last two decades have seen a warming of around 0.6°C per decade, and this is superimposed on several periods of warming and cooling over the past century. In general, over the Western English Channel domain, the end of the 20th century was around 0.5°C warmer than the first half of the century. The warming magnitude and trend is consistent with other stations across the north-west European Shelf and occurred during a period of reduced wind stress and increased levels of insolation (+20%); these are both correlated with the larger scale climatic forcing of the North Atlantic Oscillation.