Ocean Circulation in Three Dimensions
Ocean Circulation in Three Dimensions
复制标题
三维海洋环流
DOI:
10.1017/9781139015721
复制
发表时间:
2019
期刊:
影响因子:
3.2
通讯作者:
T. Haine
中科院分区:
文献类型:
--
作者:
Barry A. Klinger;T. Haine
Physical oceanography extends well beyond the study of the general ocean circulation. Physical oceanographers investigate tides, wind-driven surface waves, air/sea interaction, sound in the ocean, light in the ocean, and physical processes at the sea bed, on beaches and on man-made structures like breakwaters and ships. Physical oceanography is also key to chemical and biological oceanography, and marine geophysics. Through its coupled interaction with the atmosphere, cryosphere, biosphere, and land, the physical state of the ocean also plays a critical part in climate dynamics and Earth system science. Nevertheless, study of the ocean general circulation is central to physical oceanography and is playing a central role in the development of the field. This development involves an interplay between physical observations of the ocean, theories of the fluid dynamics, and numerical models of the circulation. The focus in this book is on the timeaveraged, global ocean currents. In order to approach this topic we must set the stage by reviewing some preliminary ideas about physical oceanography. We are selective in the coverage, only discussing topics that recur later. For comprehensive discussions of empirical methods in physical oceanography, consult the books by Emery and Thompson (2001) or Wunsch (2015). For more details on dynamical oceanography consult Vallis (2006), Marshall and Plumb (2008), or Pedlosky (1996), among others. For reflections on the field’s history, Jochem and Murtugudde (2006) and Mills (2011) are good starting points .