Titlebook: Higher Education and Police; An International Vie Colin Rogers,Bernhard Frevel Book 2018 The Editor(s) (if applicable) and The Author(s) 20

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d argue that there is considerable discursive power (Foucault 2002) in these images of the future, which explains why they are so visible and articulated with such fervor. It is not our intention to suggest that this talking about the future in and of itself constructs the future that actually unfol

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Anders Greenes as supplements to the Arctic Council and the functions of conferences for other elements in the Arctic governance regime complex. Specifically, the chapter attends to conferences as purposeful for creating synergies in the region, supporting negotiation processes, and contributing to role clarifi

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Stephen Darrochr movement. Snowmelt-driven annual maximum flow, primarily, has been decreasing, consistent with increased warming and decreased snowpack. Secondary peak flow events in late summer, driven by extreme summer rainfall and possibly enhanced by glacial melt, have been occurring more frequently in some a

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Colin Rogers,Bethan Smith Arctic temperature and sea ice. There is evidence for increased moisture content of the Arctic atmosphere and corresponding impacts on episodes of extreme warmth. The recent variations of Arctic temperature and associated variables fit well with the simulations of Arctic climate by global and regio

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Zheng Chenaturation (wetland) or storage capacity (lake). Snow is particularly important, and for Arctic wetlands and lakes, it is the total winter snow accumulation that is of major hydrological consequence. Summer rainfall in most permafrost areas is not high, and often is insufficient to match evaporation

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José-Vicente Tavares dos Santosfew Greenland fjords. The Ward Hunt Ice Shelf is the largest at about 400 km.. Arctic and Antarctic ice shelves have expanded and contracted during the Holocene. The Ellesmere Ice Shelf developed about 5500 years ago in response to Holocene cooling. In the warmer Twentieth century, calving events ha

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André Konze,Detlef Nogalaetres in length. Whether individual areas are floating in hydrostatic equilibrium or are simply close to buoyancy, they provide the major modern source of tabular icebergs to the Barents Sea. Svalbard has about 860 km of coastal ice cliffs, but almost none of the ice margin appears to be afloat. The