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systematically underestimated. The bias is not as pronounced for the non glacial rivers. Com-
bining synoptic-scale and basin-scale predictors (method 3) leads to a substantial improvement
compared to the use of MSLP fields alone (method 1). Analogue forecasts become similar or
better than persistence, depending on catchment and lead time. Usually, persistence performs
better for T=1 day and then method 3
/media/vedurstofan/utgafa/skyrslur/2013/VI_2013_008.pdf
the com-
plexity of the hydrological processes through modelling, but its application is usually limited to
the short-range. Although the results demonstrated a great potential for this method, its success-
ful application in real-time will strongly depend on the quality and availability of streamflow
observations, which can be poor or simply missing during periods of variable durations, e.g
/media/vedurstofan/utgafa/skyrslur/2014/VI_2014_006.pdf
-2049. Projections are based on simulations performed
with 18 global climate models under the SRES A1B, A2 and B1 greenhouse gas scenar-
ios.
To facilitate reading the report, only the most essential diagrams and maps are included
in the main text, additional material being positioned in the appendix.
1 MODELLED SOLAR RADIATION DATA
The quantity examined is incident solar radiation (also termed
/media/ces/CES_D2.4_solar_CMIP3.pdf