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BOGCMs, in standalone mode and coupled to fullfledged Earth system models, have been successfully used to quantify the integrated seawater column burdens of anthropogenic carbon (Figure 26.7; e.g., Assmann et al., 2010; Tjiputra et al., ...
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In reality, Γ is likely to vary with the background stratification and the strength of the turbulence (Shih et al., 2005; Ivey et al., 2008), but a discussion of these issues is beyond the purview of this chapter.
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This book presents the views of leading scientists on the knowledge of the global ocean circulation following the completion of the observational phase of the World Ocean Circulation Experiment.
A broad perspective of the ocean as a key component of the Earth System and of its role in the past, present, and future climate change is provided.
This review traces the development of in situ ocean observations primarily from a physical standpoint and describes the internationally coordinated observing networks that now supply these observations.
The ability to ascertain the implications of a changing climate are based first and foremost on our understanding the fundamental balances comprising earth’s climate.
The ocean–atmosphere exchanges of heat, water, and momentum are key elements of the global climate system.
Coupled climate models consist of atmosphere, ocean, land, and sea ice components.
In this chapter, we review the physical processes that create the mean and variable circulation features along the eastern margins of the ocean basins.
Shallow overturning cells observed in all three tropical basins as well as the deep Atlantic meridional overturning circulation are such examples that are linked to ocean and climate variations on multiple timescales.
Intensive observation programs in the North Atlantic during the past decades have demonstrated that there have been significant changes in the volumes and properties of Upper and Lower NADW as well as AABW.
The ocean has the largest heat capacity in the climate system and as a result the ocean plays a critical role in the climate.