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Hydrological responses to climate change conditioned by historic alterations of land use and water use

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Figure

Fig. 1.(b) observed and projected precipitationvalues of the GCM projections, and thick, blue lines show ensemble mean changes (reference period 1961–1990
Fig. 1c) and associated major Aral Sea shrinkage have notso far been driven by the observed historic surface climatechange within the ASDB (Shibuo et al., 2007).
Fig. 2. drological model results based on bias-corrected GCM projections
Fig. 3. Observed and projected total runoff of the principal AmuDarya and Syr Darya rivers at their Aral Sea outlets
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