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The ALADIN climate model simulation shows less than 5%% decrease for both future periods.
The model simulation shows that Mn and Fe oxyhydroxides may vary significantly along a flow path.
The ALADIN model simulation shows similar trends, however, this model projects more intensive increase of the drought hazard.
The comparison between the reported data and model simulation shows that the critical steam to carbon feed ratio predicted by the model agrees well with the reported industrial/experimental operating data.
Only minor changes were modeled, since 74 % of the arable lands were in the interval of −5 and 0% and 211 % in the interval of 0 and 5 % (Fig. 3) and the ALADIN model simulation shows the same trend for this period.
The model simulation shows that this changed direction of water flow is entirely ascribable to a change in direction of water movement via the transporter.
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A lattice model simulation showed that nonnative interactions have little effect on protein stability, but would accelerate protein folding and thus give rise to the Φ-values that are negative or larger than unity [32].
Mean integrated (0 120 m) nutrient concentrations in the whole Mediterranean basin computed from the model simulation showed different main signals for nitrate and phosphate, which are strongly correlated with the signals found in the rivers' nutrient loads (Table 2).
The model simulation showed that caspase-3 is switched ON at around t = 6000 seconds (see Figure 5, inset) and like the simple network above, there exist two activating pathways: the direct caspase-8 (type-I) and the indirect mitochondria-dependent pathway (type-II).
"The long-term climate model simulations show a trend in global-mean surface temperature from 1951 to 2012 that agrees with the observed trend (very high confidence).
The model simulations show excellent agreement with published experimental observations.
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