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起伏、拉伸和變澀模態(tài):海洋中的氣候變化(英文)

起伏、拉伸和變澀模態(tài):海洋中的氣候變化(英文)

定 價:¥298.00

作 者: 黃瑞新(Rui Xin Huang) 編
出版社: 高等教育出版社
叢編項: 全球變化與地球系統(tǒng)科學系列
標 簽: 暫缺

ISBN: 9787040542554 出版時間: 2020-10-01 包裝: 精裝
開本: 16開 頁數(shù): 391 字數(shù):  

內(nèi)容簡介

  This book is focused on fundamental aspects of climate variability in the ocean, in particular changes of the wind-driven circulation. The vertical movement of isopycnal (isothermal) layers, including their stretching and compression, is called heaving and stretching. A major part of climate vanability in the ocean is heaving in nature. Heave is primarily associated with the adiabatic motions of isopycnal layers due to change of wind stress. It is rather difficult to separate the contributions from adiabatic and diabatic processes.Isopycnal analysis has been widely used in climate study; however, it is much more accurate to study the isopycnal layers.-Here climate signals are examined in terms of changes of layer depth, layer thickness, layer temperature/salinity, spicity and others.In addition to the traditional Theta-S diagram, the sigma-pi (potential density - potential ispicity) diagram-can also be used in anatyzing water mass property distribution and climate variability. In fact, a radius of signal can be defined rigorously for signals in the sigma-pi diagram; the combination of isopycnal analysis and evaluation of radius of signal provides a powerful tool in analyzing climate variability in the world oceans.

作者簡介

暫缺《起伏、拉伸和變澀模態(tài):海洋中的氣候變化(英文)》作者簡介

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