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Box Models of Thermohaline Circulation

Box Models of Thermohaline Circulation PDF Author: Scott Li
Publisher:
ISBN:
Category :
Languages : en
Pages : 0

Book Description
This note is part of Quality testing.

Box Models of Thermohaline Circulation

Box Models of Thermohaline Circulation PDF Author: Scott Li
Publisher:
ISBN:
Category :
Languages : en
Pages : 0

Book Description
This note is part of Quality testing.

Thermohaline Circulation Stability in a Copuled Land-ocean-atmosphere Box Model

Thermohaline Circulation Stability in a Copuled Land-ocean-atmosphere Box Model PDF Author: David Michael Sirkin
Publisher:
ISBN:
Category :
Languages : en
Pages : 49

Book Description


The Effects of Resolution and Diffusion in Box Models of the Thermohaline Circulation

The Effects of Resolution and Diffusion in Box Models of the Thermohaline Circulation PDF Author: Adam Blaker
Publisher:
ISBN:
Category :
Languages : en
Pages : 59

Book Description


Thermohaline Circulation Stability

Thermohaline Circulation Stability PDF Author: Valerio Lucarini
Publisher:
ISBN:
Category :
Languages : en
Pages : 29

Book Description
Part I: A thorough analysis of the stability of the uncoupled Rooth inter-hemispheric 3-box model of thermohaline circulation (THC) is presented. The model consists of a northern high latitudes box, a tropical box, and a southern high latitudes box, which respectively correspond to the northern, tropical and southern Atlantic ocean. We adopt restoring boundary conditions for the temperature variables and flux boundary conditions for the salinity variables. We study how the strength of THC changes when the system undergoes forcings that are analogous to those of global warming conditions by applying to the equilibrium state perturbations to the moisture and heat fluxes into the three boxes. In each class of experiments, we determine, using suitably defined metrics, the boundary dividing the set of forcing scenarios that lead the system to equilibria characterized by a THC pattern similar to the present one, from those that drive the system to equilibria where the THC is reversed. Fast increases in the moisture flux into the northern high latitude box strongly inhibits the breakdown and can prevent it, in the case of slow increases in the Northern Hemisphere. Similarly, high rates of heat flux increase in the Northern Hemisphere destabilize the system more effectively than low ones, and increases in the heat fluxes in the Southern Hemisphere tend to stabilize the system.

The Oceanic Thermohaline Circulation

The Oceanic Thermohaline Circulation PDF Author: Hendrik M. van Aken
Publisher: Springer Science & Business Media
ISBN: 0387480390
Category : Science
Languages : en
Pages : 337

Book Description
This book presents a global hydrographic description of the thermohaline circulation, an introduction to the theoretical aspects of this phenomenon, and observational evidence for the theory. The hydrographic description and the observational evidence are based on data sources available via internet, mainly from the World Oceanographic Experiment (WOCE). The book also offers an introduction to hydrographic analysis and interpretation.

Interhemispheric Thermohaline Circulation in a Coupled Box Model

Interhemispheric Thermohaline Circulation in a Coupled Box Model PDF Author: Jeffery R. Scott
Publisher:
ISBN:
Category : Climatic changes
Languages : en
Pages : 44

Book Description
(Cont.) The model is augmented with explicit atmospheric eddy transport parameterizations, allowing examination of the eddy moisture transport (EMT) and eddy heat transport (EHT) feedbacks. As in the hemispheric model, the EMT feedback is always destabilizing, whereas the EHT may stabilize or destabilize. However, in this model whether the EHT stabilizes or destabilizes depends largely on the sign of the ocean salinity feedback and the size of the perturbation. Since oceanic heat transport in the southern hemisphere is weak, the northern hemisphere EMT and EHT feedbacks.

Thermohaline Circulation Stability

Thermohaline Circulation Stability PDF Author: Valerio Lucarini
Publisher:
ISBN:
Category :
Languages : en
Pages : 66

Book Description
Part I: A thorough analysis of the stability of the uncoupled Rooth inter-hemispheric 3-box model of thermohaline circulation (THC) is presented. The model consists of a northern high latitudes box, a tropical box, and a southern high latitudes box, which respectively correspond to the northern, tropical and southern Atlantic ocean. We adopt restoring boundary conditions for the temperature variables and flux boundary conditions for the salinity variables. We study how the strength of THC changes when the system undergoes forcings that are analogous to those of global warming conditions by applying to the equilibrium state perturbations to the moisture and heat fluxes into the three boxes. In each class of experiments, we determine, using suitably defined metrics, the boundary dividing the set of forcing scenarios that lead the system to equilibria characterized by a THC pattern similar to the present one, from those that drive the system to equilibria where the THC is reversed. Fast increases in the moisture flux into the northern high latitude box strongly inhibits the breakdown and can prevent it, in the case of slow increases in the Northern Hemisphere. Similarly, high rates of heat flux increase in the Northern Hemisphere destabilize the system more effectively than low ones, and increases in the heat fluxes in the Southern Hemisphere tend to stabilize the system.

Presenting and Scrutinising a New Box Model for Interhemisphere Thermohaline Circulation

Presenting and Scrutinising a New Box Model for Interhemisphere Thermohaline Circulation PDF Author: Jacob Royle
Publisher:
ISBN:
Category :
Languages : en
Pages : 56

Book Description


Oceanic Circulation Models: Combining Data and Dynamics

Oceanic Circulation Models: Combining Data and Dynamics PDF Author: D.L.T. Anderson
Publisher: Springer Science & Business Media
ISBN: 9400910134
Category : Science
Languages : en
Pages : 616

Book Description
This book which is the outcome of a NATO-Advanced Study Institute on Mod elling the Ocean Circulation and Geochemical Tracer Transport is concerned with using models to infer the ocean circulation. Understanding our climate is one of the major problems of the late twentieth century. The possible climatic changes resulting from the rise in atmospheric carbon dioxide and other trace gases are of primary interest and the ocean pla. ys a ma. jor role in determining the magnitude, temporal evolution and regional distribution of those changes. Because of the poor observational basis the ocean general circulation is not well understood. The World Ocean Circulation Experiment (WOCE) which is now underway is an attempt to improve our knowledge of ocean dynamics and thermodynamics on global scales relevant to climate change. Despite those efforts, the oceanic data base is likely to remain scarce and it is crucial to use appropriate methods in order to extract the maximum amount of information from observations. The book contains a thorough analysis of methods to combine data of val'ious types with dynamical concepts, and to assimilate data directly into ocean models. The properties of geocl;temical tracers such as HC, He, Tritium and Freons and how they may be used to impose integral constraints on the ocean circulation are discussed.

Ocean Circulation and Climate

Ocean Circulation and Climate PDF Author: Sybren S. Drijfhout
Publisher: Elsevier Inc. Chapters
ISBN: 0128058609
Category : Science
Languages : en
Pages : 68

Book Description
Conceptual models are a vital tool for understanding the processes that maintain the global ocean circulation, both in nature and in complex numerical ocean models. In this chapter we provide a broad overview of our conceptual understanding of the wind-driven circulation, the thermohaline circulation, and their transient behavior. While our conceptual understanding of the time-mean wind-driven circulation is now fairly mature, basic questions remain regarding the thermohaline circulation, for example, surrounding its overall strength and stability. Similarly, basic questions remain regarding the transient adjustment and internal variability of the ocean circulation.