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the numerical model of the biosphere which would simulate the dependences of
biospheric components on climate parameters. In the
first case, unstable solutions of
respective systems of differential equations appear problematical, which hinders
prognostic estimates of global environmental change. In the second case, there is a
probability to obtain stable forecasts of environmental change, but their reliability
depends on the accuracy of parameterization of correlations between elements of
the biosphere and climate. The second approach has the advantage of incorporating
models which can be described at a scenario level.
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