"climate equilibrium" is a correct and usable phrase in written English.
You can use it to refer to a point or state of balance between different factors in the global climate. For example, "Scientists are striving to maintain a climate equilibrium that will enable the survival of all species."
This increase in heat seriously threatens the global climate equilibrium that determines the patterns of winds, rainfall, surface temperatures, ocean currents, and sea level.
In addition to bio-fuel, could hemp also lead to other benefits --- like helping restore the earth's climate equilibrium?
A draft seen by the Guardian warns that the "vegetation-climate equilibrium is teetering on the brink of the abyss".
Uncertainty in equilibrium climate sensitivity (ECS), determined by global mean surface air temperature (SAT) increase at a state of climatic equilibrium according to doubling of atmospheric CO2, is an unresolved issue in the climate science (e.g., Knutti and Hegerl 2008).
The behavior of the overall control action is evaluated using an uncertainty scenario for climate model equilibrium sensitivity.
Fig. 1 Equilibrium climate sensitivity (ECS) and transient climate response (TCR) of 23 Cmodelsodels.
It also asked what the Energy Department considers to be "the proper equilibrium climate sensitivity," which is a way climate researchers calculate how much the planet will eventually warm, depending on the amount of greenhouse gases emitted into the atmosphere.
An international team of researchers looked at how the last decade would impact long-term, equilibrium climate sensitivity and the shorter term climate response.
While predicted equilibrium climates from three climate models (MIT 2D, GISS and GFDL GCMs) have been used in both cases, predicted soil organic carbon from terrestrial ecocystem model (TEM, Melillo et al., 1993) have been used in the "doubled-CO2" case and CLIMAP data (1981) have been used in the "ice age" case.
The equilibrium climate sensitivity (ECS) - the response of the climate to a doubling of CO2 in the atmosphere - is likely to result in a change of between 1.5C and 4.5C.
An "equilibrium climate experiment" is an experiment in which a climate model is allowed to fully adjust to a change in radiative forcing.
