Not exact matches
Broecker, W.S., 1997:
Thermohaline circulation, the Achilles heel of our climate
system: will man - made CO2 upset the current balance?
[I] n the Atlantic, the heat is carried north as part of a powerful current
system known as the Atlantic
thermohaline circulation.
In the ocean, we need to consider better the controls on
thermohaline circulation, on potential changes in biological productivity, and on the overall stability of the ocean
circulation system.
We have used the Grid ENabled Integrated Earth
system modelling (GENIE) framework to undertake a systematic search for bi-stability of the ocean
thermohaline circulation (THC) for different surface grids and resolutions of 3 - D ocean (GOLDSTEIN) under a 3 - D dynamical atmosphere model (IGCM).
Pachauri outlined the potential for major changes to the climate
system, which could overwhelm human response strategies - breakdown of the
thermohaline circulation, disintegration of the West Antarctic Ice Sheet, a shift in mean climate towards an El Nino - like state, reduced carbon sink capacity, methane release from hydrates, and a rearrangement of biome distributions.
In recent decades, much research on these topics has raised the questions of «tipping points» and «
system flips,» where feedbacks in the
system compound to rapidly cause massive reorganization of global climate over very short periods of time — a truncation or reorganization of the
thermohaline circulation or of food web structures, for instance, caused by the loss of sea ice or warming ocean temperatures.
So far, we know of only one element of the climate
system which has multiple modes of operation: the oceans»
thermohaline circulation.
The natural internal variability of the climate
system arises from factors such as El Niño, fluctuations in the
thermohaline circulation, and changes in ocean heat content.
· Freshwater influx from movements and melting of sea ice or ice sheets may lead to a weakening of the global
thermohaline circulation, causing unpredictable instabilities in the climate
system.
• Freshwater influx from the movements and melting of sea ice or ice sheets may lead to a weakening of the global
thermohaline circulation, causing unpredictable instabilities in the climate
system.
...
system known as the «
thermohaline circulation» or «great ocean conveyor belt.»