thermohaline circulation

He is also known for his work on thermohaline circulation.

One of the obvious places to start here was with the thermohaline circulation stall.

Another possibility is that there was a slowing of thermohaline circulation.

Changes in the thermohaline circulation are thought to have significant impacts on the earth's radiation budget.

Hence it is difficult in this case to subduct water through the thermohaline circulation.

This is the beginning of the thermohaline circulation.

He keeps an eye on environmental triggers such as climate change in the Arctic and thermohaline circulation.

Thermohaline circulation may be altered by increasing amounts of freshwater in the ocean.

A major controlling factor in oceanic-atmospheric carbon exchange is thermohaline circulation.

Upwelling is the opposite process and together these two forces are responsible in the oceans for the thermohaline circulation.

All the data, Kenzo explained, indicated stalls in what he called the "thermohaline circulation."

Stommel also developed early models of the thermohaline circulation which suggested that it might have more than one stable state.

Thermohaline circulation is the principal driving force of deepwater bottom-currents.

While a number of processes drive thermohaline circulation, there are a few that are unique to the Arctic.

Early work with simplified models suggested that global warming could cause a shutdown of the thermohaline circulation.

In this way, the thermohaline circulation can be considered to have been less "thermo" and more "haline".

Then also thermohaline circulation, in particular the North Atlantic stall in the great world current.

There is some concern that a shutdown of thermohaline circulation could happen again as a result of the present warming period.

Thermohaline circulation exchanges carbon between these two layers.

Thermohaline circulation - the global density-driven circulation of the oceans.

This is called a thermohaline circulation.

Internal forcing mechanisms are natural processes within the climate system itself (e.g., the thermohaline circulation).

Thermohaline circulation is responsible for bringing up cold, nutrient rich water from the depths of the ocean, a process known as upwelling.

An abrupt shutdown of thermohaline circulation causes catastrophic climate change, plunging the Earth into a new ice age.

Another phytoplankton bloom occurs more to the north near the antarctic convergence, here nutrients are present from thermohaline circulation.