In this chapter, we review the physical processes that create the mean and variable circulation features along the eastern margins of the ocean basins. Rather than describing the individual systems, we describe the processes and their variability between the systems, dividing the discussion into the low-, mid- and high-latitude regions. We start with the low latitudes, since their signals often move poleward along the coastal wave guides into the midlatitudes, which are the well-known eastern boundary upwelling systems. Our treatment of the higher latitudes is limited to examples from the better-studied NE Pacific Basin (The Alaska Current).
The book represents all the knowledge we currently have on ocean circulation.
In: Goni, G.J., Malanotte-Rizzoli, P. (Eds.), Interhemispheric Water Exchange in the Atlantic Ocean. Elsevier Oceanogr. Ser., vol. 68. Elsevier, Amsterdam, pp. 411–442, Chapter 16. Johnson, G.C., Zhang, D., 2003.
OpenAD/F: a modular, opensource tool for automatic differentiation of Fortran codes. ACM Trans Math Softw. ... Vinogradova NT, Ponte RM, Tamisiea ME, Quinn KJ, Hill EM, Davis JL. Selfattraction and loading effects on ocean mass ...
Frankignoul C, Sennéchael N. Observed influence of North Pacific SST anomalies on the atmospheric circulation. J Clim. 2007;20:592–606. ... Fratantoni DM, Bower AS, Johns WE, Peters H. Somali Current rings in the eastern Gulf of Aden.
An inherent feature of the climate is its strong variability on a vast range of timescales, from seasonal to multimillennial and beyond.
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The Southern Ocean circulation connects the ocean basins as well as the upper and deep layers of the ocean. As a result, the region has a profound influence on the global ocean circulation and climate.
The book moves smoothly from fundamental principles to topics of current research interest, including natural climate variability, such as El Ni o, and the daunting challenge of man-made climate change, or global warming.
The book comprises chapters covering distinct aspects of contrasting ocean currents: broad and slow, deep and shallow, narrow and swift, large scale and small scale, low latitudes and high latitudes, and moving in horizontal and vertical ...
In The Great Ocean Conveyor, Broecker introduces readers to the science of abrupt climate change while providing a vivid, firsthand account of the field's history and development.