887 resultados para Space debris Law and legislation


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After many meetings and long hours of negotiations, the overwhelming feeling when a deal between the EU and Turkey was struck, was one of “mission accomplished”! Faced with an unprecedented crisis and forced to appease increasingly hostile public opinions back home, EU leaders had only one objective in mind: reducing the number of migrants arriving in the EU so that order can return in the framework of EU rules. However, a closer look at the Summit Conclusions and the EU-Turkey statement leaves a bitter taste, according to Yves Pascouau. In this Commentary, he questions the feasibility of the final EU-Turkey deal, saying that it creates more problems than it solves: besides the obvious legal and practical issues, it is far from certain which member states will be willing to do their part, or whether or not the EU can come up with a strategic vision on human mobility for the future.

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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 negotiation of a patchy but burgeoning network of international investment agreements and the increasing use to which they are put is generating a growing body of jurisprudence which, while still evolving, requires closer analytical scrutiny. Drawing on many of the most distinguished voices in investment law and policy, and offering novel, multidisciplinary perspectives on the rapidly evolving landscape shaping international investment activity and treaty-making, this book explores the most important economic, legal and policy challenges in contemporary international investment law and policy. It also examines the systemic implications flowing from frenetic recent judicial activism in investment matters and advances several innovative propositions for how best to promote greater overall coherence in rule-design, treaty use and policy making and thus offer a better balance between the rights and obligations of international investors and host states.

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Ice-rafted debris (IRD) (>2 mm), input in eight sediment cores along the Eurasian continental margin (Arctic Ocean), have been studied over the last two glacial/interglacial cycles. Together with the revised chronologies and new micropaleontological data of two cores from the northern Barents Sea (PS2138) and northeastern Kara Sea (PS2741) spanning Marine Isotope Stages (MIS) 6 to 1, the IRD data give new insights into the glacial history of northern Eurasian ice-sheets over the last 150 ka. The chronologies of the cores are based on stable isotope records, AMS 14C datings, paleomagnetic and biostratigraphic data. Extensive episodes of northern Barents Sea ice-sheet growth, probably to the shelf edge, occurred during the late Weichselian (MIS 2) and the Saalian (MIS 6). Major IRD discharge at the MIS 4/3-transition hints to another severe glaciation, probably onto the outer shelf, during MIS 4. IRD-based instabilities of the marine-based ice margin along the northern Barents Sea between MIS 4 and 2 are similar in timing with North Atlantic Heinrich events and Nordic Seas IRD events, suggesting similar atmospheric cooling over a broad region or linkage of ice-sheet fluctuations through small sea-level events. In the relatively low-precipitation areas of eastern Eurasia, IRD peak values during Termination II and MIS 4/3-transition suggest a Kara Sea ice-sheet advance onto the outer shelf, probably to the shelf edge, during glacial MIS 6 and 4. This suggests that during the initial cooling following the interglacials MIS 5, and possibly MIS 7, the combined effect of sustained inflow of Atlantic water into the Arctic Ocean and penetration of moisture-bearing cyclones into easterly direction supported major ice build-up during Saalian (MIS 6) and Mid-Weichselian (MIS 4) glaciation. IRD peak values in MIS 5 indicate at least two advances of the Severnaya Semlya ice-sheet to the coast line during the Early Weichselian. In contrast, a distinct Kara Sea ice advance during the Late Weichselian (MIS 2) is not documented by the IRD records along the northeastern Kara Sea margin.

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Oxygen isotope records, radiocarbon AMS data, carbonate and opal stratigraphy, sediment magnetic susceptibility, tephrachronology, and paleontological results were used to obtain detailed sediment stratigraphy and an age model for the studied cores. For studying sea-ice sedimentation an analysis of lithogenic grain number in >0.15 mm grain size fraction of bottom sediments was carried out. For quantitative estimation of intensity ice-rafting debris sedimentation number of IRD particles per sq cm per ka was calculated. Obtained results allowed to plot IRD AR distribution for the first oxygen isotope stage (0-12.5 14C ka, 14C) and for the second stage (12.5-24 14C ka). The first stage was subdivided into the latest deglaciation and the beginning of Holocene (6-12.5 14C ka) (transitive period), when the sea level was changing significantly, and the second part of Holocene (0-6 14C ka), when climate conditions and the sea level were similar to modern estimates. Data clearly show strong increase in ice formation in the glacial Sea of Okhotsk and its extent in the middle part of the sea. Average annual duration of ice coverage during glaciation was longer than that for interglaciation. However the sea ice cover was not continuous all the year round and disappeared in summer time except the far northwestern part of the sea.

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Includes bibliographical references.

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Paged continuously.

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Mode of access: Internet.

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"A Law-Institute of the Americas study."

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Mode of access: Internet.