Strong, persistent currents along the western boundaries of the world’s major ocean basins are called “western boundary currents” (WBCs). This chapter describes the structure and dynamics of WBCs, their roles in basin-scale circulation, regional variability, and their influence on atmosphere and climate. WBCs are largely a manifestation of wind-driven circulation; they compensate the meridional Sverdrup transport induced by the winds over the ocean interior. Some WBCs also play a role in the global thermohaline circulation, through inter-gyre and inter-basin water exchanges. After separation from the boundary, most WBCs have zonal extensions, which exhibit high eddy kinetic energy due to flow instabilities, and large surface fluxes of heat and carbon dioxide. The WBCs described here in detail are the Gulf Stream, Brazil and Malvinas Currents in the Atlantic, the Somali and Agulhas Currents in the Indian, and the Kuroshio and East Australian Current in the Pacific Ocean.
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.
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 ...
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.
This is the first book to deal with all aspects of the ocean's large-scale meridional overturning circulation, and is a coherent presentation, from a mechanistic point of view, of our current understanding of paleo, present-day, and future ...