970 resultados para Offer calculation
EC tables detailed market access offer in Geneva. European Community News No. 55/93, 22 October 1993
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On the basis of the success of the two previous waves of European Union enlargement to post-communist states, EU accession is the international community's solution for ending the state-building impasse in Bosnia and Herzegovina. Through a literature review of analysis of the recent EU enlargements, this paper compares those countries' experiences with the current situation in Bosnia, and raises questions about the ability of the EU to address state-building issues through the accession process. The paper concludes that the previous enlargements do not provide a model for state-building in Bosnia. Because the EU's attempts to help along the process of state building in Bosnia is a new type of policy project, the paper proposes how the enlargement process might be adapted to address the specific problems in Bosnia, particularly in terms using human rights norms to compel Bosnian leaders to adopt necessary reforms.
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Poster apresentado no Congresso O Norte da Anestesia, 19-21 Novembro 2015, Hotel Ipanema Park, Porto, Portugal.
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High-resolution records of carbon and oxygen isotopes and benthic foraminiferal accumulation rates for the Eocene-Oligocene section at Ocean Drilling Program Site 689 (Maud Rise, Weddell Sea; paleodepth about 1500 m) were used to infer variations in paleoproductivity in relation to changes in climate and ventilation of the deeper-water column. The benthic foraminiferal abundance and isotope records show short-term fluctuations at periodicities of 100 and 400 ka, implying orbitally driven climatic variations. Both records suggest that intermediate-depth water chemistry and primary productivity changed in response to climate. During the Eocene, productivity increased during cold periods and during cold-to-warm transitions, possibly as a result of increased upwelling of nutrient-rich waters. In the Oligocene, in contrast, productivity maxima occurred during intervals of low delta18O values (presumably warmer periods), when a proto-polar front moved to the south of the location of Site 689. This profound transition in climate-productivity patterns occurred around 37 Ma, coeval with rapid changes toward increasing variability of the oxygen and carbon isotope and benthic abundance records and toward larger-amplitude delta18O fluctuations. Therefore, we infer that, at this time, temperature fluctuations increased and a proto-polar front formed in conjunction with the first distinct pulsations in size of the Antarctic ice sheet. We speculate that this major change might have resulted from an initial opening of the Drake Passage at 37 Ma, at least for surface- and intermediate-water circulation.
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The molecular stratigraphy of Biogeochemical Oceanic Flux Study core 31K (19°N, 20°10'W) and Ocean Drilling Program Hole 658C (20°45'N, 18°35'W) has been studied for C37 alkenone abundances over the past 80 ka at high resolution (~circa 200-500 years). The derived Uk 37' sea surface temperature record for both cores shows a range of temperatures from about 18°C during the last glacial to 21.5°C during the early Holocene. Both records also reveal changes in sea surface temperature as much as 2°-4°C over a few hundred years, which correlate well with similar abrupt climatic changes observed in cores from elsewhere in the NE Atlantic, associated with 'Heinrich events'. Our results indicate that meltwater produced by these ice-rafting events was transmitted southward by the Canary Current, where it had considerable impact on sea surface temperatures in the subtropical eastern Atlantic.
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"Office of the Assistant Secretary for Policy Development and Research, Dept. of Housing and Urban Development."
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Mode of access: Internet.