scispace - formally typeset
Journal ArticleDOI

On the freshwater forcing and transport of the Atlantic thermohaline circulation

Stefan Rahmstorf
- 01 Nov 1996 - 
- Vol. 12, Iss: 12, pp 799-811
Reads0
Chats0
TLDR
In this article, it is argued that the freshwater loss to the atmosphere arises mainly in the subtropical South Atlantic and is balanced by northward freshwater transport in the wind-driven sub-tropical gyre, while the thermohaline circulation transports freshwater southward.
Abstract
The 'conveyor belt' circulation of the Atlantic Ocean transports large amounts of heat northward, acting as a heating system for the northern North Atlantic region. It is widely thought that this circulation is driven by atmospheric freshwater export from the Atlantic catchment region, and that it transports freshwater northward to balance the loss to the atmosphere. Using results from a simple conceptual model and a global circulation model, it is argued here that the freshwater loss to the atmosphere arises mainly in the subtropical South Atlantic and is balanced by northward freshwater transport in the wind-driven subtropical gyre, while the thermohaline circulation transports freshwater southward. It is further argued that the direction of freshwater transport is closely linked to the dynamical regime and stability of the 'conveyor belt': if its freshwater transport is indeed southward, then its flow is purely thermally driven and inhibited by the freshwater forcing. In this case the circulation is not far from Stommel's saddle-node bifurcation, and a circulation state without NADW formation would also be stable.

read more

Content maybe subject to copyright    Report

Citations
More filters
Dissertation

Early warning signals of environmental tipping points

TL;DR: Early warning signals of Atlantic Meridional Overturning Circulation Collapse in a Fully Coupled Climate Model (FCCM) were used in this paper to identify the tipping points in the climate system.
Dissertation

Abrupt climate change and glacialterminations

Emily Deaney
TL;DR: The authors investigated the shorter millennial scale events (thousands of years) and their role in determining the magnitude of glacial-interglacial cyclicity using sediment cores from the North and South Atlantic.
Posted ContentDOI

Bjerknes compensation in a coupled global box model

TL;DR: The probability of a valid BJC is usually very high under reasonable climate feedback, which is found to be robust in the real world based on observational data, implying that the Earth climate system maintains it energy balance very well during the past one hundred years.
Dissertation

Evaluation of modeling ecosystem seasonality in the University of Victoria Earth System Climate Model

Annika Eisele
TL;DR: In this article, the authors evaluated the accuracy of the University of Victoria Earth System climate model (UVic model) simulations of timing, forcing factors and limitations (e.g. mixed layer depth, temperature, irradiance, nutrients, zooplankton grazing pressure) to the North Atlantic spring bloom, model output has been compared to observations from MODIS satellite images, WOA09 data, IFREMER records and PAP measurements.

Response of the Atlantic Thermohaline Circulation to Changes of Atmospheric Green House Gases

Yang Haijun
TL;DR: In this paper, the equilibrium response of the thermohaline circulation (THC) to changes of atmospheric Green House Gases is simulated using a fully coupled climate model, where the response is divided into two different stages: the transient stage and the equilibrium stage.
References
More filters

Climatological atlas of the world ocean

TL;DR: A project to objectively analyze historical ocean temperature, salinity, oxygen, and percent oxygen saturation data for the world ocean has recently been completed at the National Oceanic and Atmospheric Administration's (NOAA) Geophysical Fluid Dynamics Laboratory, Princeton, New Jersey.
Book

Climatological Atlas of the World Ocean

TL;DR: A project to objectively analyze historical ocean temperature, salinity, oxygen, and percent oxygen saturation data for the world ocean has recently been completed at the National Oceanic and Atmospheric Administration's (NOAA) Geophysical Fluid Dynamics Laboratory, Princeton, New Jersey.
Journal ArticleDOI

Normal Monthly Wind Stress Over the World Ocean with Error Estimates

TL;DR: In this paper, wind and air-minus-sea temperatures are calculated in a form suitable for determining stress by any bulk aerodynamics model in which the drag coefficient can be represented by six or less coefficients of a second-degree polynomial in wind speed and stability.
Journal ArticleDOI

Interocean Exchange of Thermocline Water

TL;DR: In this paper, it is proposed that this return flow is accomplished primarily within the ocean's warm water thermocline layer, where the main thermoclines of the ocean are linked as they participate in a thermohaline-driven global scale circulation cell associated with NADW formation.
Journal ArticleDOI

The Great Ocean Conveyor

Wallace Broeker
- 01 Jan 1991 - 
TL;DR: The ocean's conveyor appears to be driven by the salt left behind as the result of water-vapor transport through the atmosphere from the Atlantic to the Pacific basin this paper.
Related Papers (5)