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Titlebook: Arctic-Subarctic Ocean Fluxes; Defining the Role of Robert R. Dickson,Jens Meincke,Peter Rhines Book 2008 Springer Science+Business Media B

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The Changing View on How Freshwater Impacts the Atlantic Meridional Overturning Circulation,on (AMOC) contributes effectively to the anomalous warmth of northern Europe (Large and Nurser 2001; see also Rhines and Hakkinen 2003; Rhines et al., this volume). The oceanic fluxes of mass, heat and salt that pass north across the Greenland–Scotland Ridge from the Atlantic to the Arctic Mediterra
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Constraints on Estimating Mass, Heat and Freshwater Transports in the Arctic Ocean: An Exercise,Bay and the Labrador Sea –, also provides an opportunity to examine the mass (volume), freshwater and heat budgets of the Arctic Ocean. The exchanges between the two passages between the Arctic Ocean and the Nordic Seas, Fram Strait and the Barents Sea opening between Norway and Bear Island, have be
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Simulating the Terms in the Arctic Hydrological Budget,ate of transport in cubic kilometer per year carried by the individual branches. Bold numbers are observational estimates taken from Aagaard and Carmack (1989), Carmack (2000) and Woodgate and Aagaard (2005), while other numbers are taken from freshwater budget analysis of several century long clima
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Is the Global Conveyor Belt Threatened by Arctic Ocean Fresh Water Outflow?,ons and pathways of fresh water. Most fresh water within the Arctic Ocean occurs as a result of there being more evaporation than precipitation in the Atlantic Ocean. Much of the excess evaporation from the Atlantic Ocean falls as rain into the Pacific Ocean and into river drainage basins that feed
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Simulating the Long-Term Variability of Liquid Freshwater Export from the Arctic Ocean,s not easily accessible for oceanographic vessels and so far has been off-limits for moored instrumentation. Even if we would be able to start measurements now, we would have no statistics to evaluate trends and natural variability of the transport. For long time series and for predictions of future
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