terrestrial biosphere

Carbon leaves the terrestrial biosphere in several ways and on different time scales.

The question is are the natural sinks like the terrestrial biosphere able to keep that up?"

Opponents feared that the terrestrial biosphere would be used as an escape route.

Atmospheric carbon is exchanged quickly between the oceans and the terrestrial biosphere.

Over the long run, fossil fuel emissions can not be compensated for by the terrestrial biosphere.

During the 1980s it became increasingly clear that the terrestrial biosphere played an important part in terms of the global atmospheric carbon balance.

The four sinks are the atmosphere, terrestrial biosphere, oceans and sediments.

Human activity has large effects on the terrestrial biosphere, changing the way that it acts as a carbon reservoir.

The more active carbon storage areas within the Earth’s ecosystem are the living terrestrial biosphere, the atmosphere and the oceans.

Heimann (2002) Assimilating atmospheric data into a terrestrial biosphere model.

Carbon budget and modelling of the terrestrial biosphere.

Land cover change greatly decreases the amount of carbon uptake in the terrestrial biosphere.

Carbon is exchanged with varying speed with the terrestrial biosphere.

Does the terrestrial biosphere have planetary tipping points?

Carbon in the terrestrial biosphere enters the geosphere only through highly specialized processes.

Terrestrial biosphere and climate affect each other.

Most carbon leaves the terrestrial biosphere through respiration.

Soil carbon A major component of the terrestrial biosphere pool in the carbon cycle.

The residence time of carbon in the terrestrial biosphere varies and is dependent on a large number of factors.

This in turn, may reflect an increase in methane production and subsequent release from the terrestrial biosphere."

Will the natural system continue to absorb more than 50% of the human release of carbon dioxide into the terrestrial biosphere and oceans?

The vegetation had the wild look of a kzinti hunting park, with pink and orange blended into the imported terrestrial biosphere.

Detecting a terrestrial biosphere sink for carbon dioxide:

Also the opponents stated that the uncertainties in the terrestrial biosphere are still so great that the results achieved could not be verified.

Modeling the global carbon cycle: nitrogen fertilization of the terrestrial biosphere and the "missing" CO2 sink.