Dima belkin biography of christopher
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2010: Dmitrij Belkin- "Gaste, die bleiben": Vladimir Solov'ev, die Juden und die Deutschen
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Zakhar Ishov
Refubium, 2009
In the present thesis I will set to investigate Brodsky’s translating methods with the idea of trying to assign them a place within both English literature as well as the practice of poetical translation into the English language. Because of the paucity of research dedicated to Brodsky’s self-translation so far, as well as the tendency, which has persisted for over a decade following Brodsky’s untimely death in 1996 in the few existing articles and scholarly works on the subject to trade in opinions, I felt the need for a change of the critical approach in the field of Brodsky’s self-translations. For the first time in the history of this field, I will dedicate some of these translations a detailed textual analysis with the aim of establishing on concrete examples Brodsky’s exact translational procedures and to try to make their assessment within practices of English poetry translation. My inquiry has been immensely enriched by the fact that the new availability of research materials of
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Opportunities for Earth Observation to Inform Risk Management for Ocean Tipping Points
2.1 Atlantic Meridional Overturning Circulation (AMOC)
2.1.1 Nature of Tipping Point
The Atlantic Meridional Overturning Circulation (AMOC) is a global-scale system of currents which transports warm water northwards in the Atlantic Basin. Much of the heat is lost to the atmosphere in the North Atlantic high latitudes, and consequently the AMOC has a fundamental role in shaping Northern Hemisphere climate (e.g. Bonnet et al. 2021). The AMOC is often characterised as a global-scale ‘conveyor belt’ circulation (Broecker 1991), driven by heat and fresh water exchanges with the atmosphere, and the consequent density changes. While this view is undoubtedly a gross simplification, model studies suggest that on decadal and longer timescales, coherent basin- or global-scale variations in the circulation are possible. In this section, we focus on large-scale variations whereas North Atlantic subpolar gyre variability is discussed in Sect. 2.2.
The AMOC has been long recognised as one of the major tipping elements of the climate system (Stommel 1961; Rooth 1982; Rahmstorf 1996, Lenton et al 2008 Swingedouw 2020; Armstrong McKay et al. 2022; Boers et al 2022). AMOC transitions (tipping) and multiple
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57th Competition – 2021
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