Author: Rui Xin Huang
Publisher: Springer Nature
ISBN: 9811529418
Category : Science
Languages : en
Pages : 399
Book Description
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 variability 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 spicity) diagram can also be used in analyzing 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.
Heaving, Stretching and Spicing Modes
Author: Rui Xin Huang
Publisher: Springer Nature
ISBN: 9811529418
Category : Science
Languages : en
Pages : 399
Book Description
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 variability 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 spicity) diagram can also be used in analyzing 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.
Publisher: Springer Nature
ISBN: 9811529418
Category : Science
Languages : en
Pages : 399
Book Description
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 variability 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 spicity) diagram can also be used in analyzing 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.
Heaving, Stretching and Spicing Modes
Author: Rui Xin Huang
Publisher:
ISBN: 9787040542554
Category : Marine meteorology
Languages : en
Pages : 391
Book Description
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 variability 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 spicity) diagram can also be used in analyzing 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.
Publisher:
ISBN: 9787040542554
Category : Marine meteorology
Languages : en
Pages : 391
Book Description
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 variability 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 spicity) diagram can also be used in analyzing 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.
Ocean Circulation
Author: Rui Xin Huang
Publisher: Cambridge University Press
ISBN: 0521852285
Category : Science
Languages : en
Pages : 807
Book Description
It provides a concise introduction to the dynamics and thermodynamics of oceanic general circulation.
Publisher: Cambridge University Press
ISBN: 0521852285
Category : Science
Languages : en
Pages : 807
Book Description
It provides a concise introduction to the dynamics and thermodynamics of oceanic general circulation.
Zonal Jets
Author: Boris Galperin
Publisher: Cambridge University Press
ISBN: 1107043883
Category : Nature
Languages : en
Pages : 527
Book Description
Presents a comprehensive, multidisciplinary volume on the physics of zonal jets, from the leading experts, for graduate students and researchers.
Publisher: Cambridge University Press
ISBN: 1107043883
Category : Nature
Languages : en
Pages : 527
Book Description
Presents a comprehensive, multidisciplinary volume on the physics of zonal jets, from the leading experts, for graduate students and researchers.
New York Journal of Romance, General Literature, Science and Art
Acceptable Methods, Techniques, and Practices
The Ancient Régime
Author: Hippolyte Taine
Publisher:
ISBN:
Category : History
Languages : en
Pages : 442
Book Description
Publisher:
ISBN:
Category : History
Languages : en
Pages : 442
Book Description
The Origines of Contemporary France
The Origins of Contemporary France: The ancient régime
Author: Hippolyte Taine
Publisher: New York : H. Holt, 1890- [v. 1
ISBN:
Category : France
Languages : en
Pages : 452
Book Description
Publisher: New York : H. Holt, 1890- [v. 1
ISBN:
Category : France
Languages : en
Pages : 452
Book Description