804 resultados para Copenhagen


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The European Union, together with all countries, is making a second effort to reach a comprehensive global climate change agreement at the United Nations Climate Change Conference (COP21 or CMP11) in Paris in December 2015, after the unsuccessful attempt to do so in Copenhagen in 2009. At a time when the EU is still preoccupied with recovery from the economic crisis, and is facing geopolitical challenges and a number of conflicts, why should it see the importance of continuing to offer leadership in the field of climate change? And why would such an agreement be important for the EU? In short: “What’s in it for the EU?” This commentary reviews the wider context of the negotiations, looking not only at the geopolitical shifts that have taken place on the road to Paris, but also at the interests of the EU both as far as its domestic climate policy is concerned, as well as its role as a diplomatic ‘soft power’.

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The European Union is founded on a set of common principles of democracy, the rule of law, and fundamental rights, as enshrined in Article 2 of the Treaty on the European Union. Whereas future Member States are vetted for their compliance with these values before they accede to the Union, no similar method exists to supervise adherence to these foundational principles after accession. EU history proved that this ‘Copenhagen dilemma’ was far from theoretical. EU Member State governments’ adherence to foundational EU values cannot be taken for granted. Violations may happen in individual cases, or in a systemic way, which may go as far as overthrowing the rule of law. Against this background the European Parliament initiated a Legislative Own-Initiative Report on the establishment of an EU mechanism on democracy, the rule of law and fundamental rights and proposed among others a Scoreboard on the basis of common and objective indicators by which foundational values can be measured. This Research Paper assesses the need and possibilities for the establishment of an EU Scoreboard, as well as its related social, economic, legal and political ‘costs and benefits’.

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The Danish Expedition of the "Galathea II" around the world brought important results concerning the marine organisms in the deep sea. The "Galathea II" showed not only different organisms of the Abyssal but for the first time of the deepest trenches of the western Pacific. Anton Bruun coined the term Hadal for the region below the Abyssal under 6000 m. Although the "Galathea II" aimed to investigate new deep sea regions beside the routes of former expeditions and to widen the horizon of knowledge relating marine organisms the technical equipment and the methodological approach had partly been developed earlier. The expedition of the "Galathea II" is part of a long tradition of cruises such as that of the British "Challenger", the German "Valdivia" and the Swedish "Albatross" and especially the Danish cruises of the "Dana I" and "Dana II" which happened some years before.

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The work in this sub-project of ESOP focuses on the advective and convective transforma-tion of water masses in the Greenland Sea and its neighbouring areas. It includes observational work on the sub-mesoscale and analysis of hydrographic data up to the gyre-scale. Observations of active convective plumes were made with a towed chain equipped with up to 80 CTD sensors, giving a horizontal and vertical resolution of the hydrographic fields of a few metres. The observed scales of the penetrative convective plumes compare well with those given by theory. On the mesoscale the structure of homogeneous eddies formed as a result of deep convection was observed and the associated mixing and renewal of the intermediate layers quantified. The relative importance and efficiency of thermal and haline penetrative convection in relation to the surface boundary conditions (heat and salt fluxes and ice cover) and the ambient stratification are studied using the multi year time series of hydro-graphic data in the central Greenland Sea. The modification of the water column of the Greenland Sea gyre through advection from and mixing with water at its rim is assessed on longer time scales. The relative contributions are quantified using modern water mass analysis methods based on inverse techniques. Likewise the convective renewal and the spreading of the Arctic Intermediate Water from its formation area is quantified. The aim is to budget the heat and salt content of the water column, in particular of the low salinity surface layer, and to relate its seasonal and interannual variability to the lateral fluxes and the fluxes at the air-sea-ice interface. This will allow to estimate residence times for the different layers of the Greenland Sea gyre, a quantity important for the description of the Polar Ocean carbon cycle.

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Series numbering dropped with: <1967>.

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Mode of access: Internet.

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Original imprint covered by label which reads; A. A. Knopf, New York.

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Description based on: 15. nov. 1960.

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1906/07-1961/62: Saertryk af Tidsskrift for planteavl.

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Editor:<1968>- Foreningen Fremtiden.

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"Udgivet paa bekostning af Carlsbergfondet."

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1.Stratomyiidae Xylophagidae, Coenomyiidae, Tabanidae, Leptididae, Acroceridae.-2. Asilidae, Bombyliidae, Therevidae, Scenopinidae.-3. Empididae.-4. Dolichopodidae.-5. Lonchopteridae, Syrphidae.-6. Pipunculidae, Phoridae.-7. Platypezidae, tachinidae.

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Vol. 3-4, pt. 1. udg. af C. Plesner; v. 4, [pt. 2]: Register, udg af A. Thiset; v. 5, "ved William Christensen."

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Title varies.