Directory UMM :Data Elmu:jurnal:A:Advances In Water Resources:Vol21.Issue8.1998:
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This poor situation takes a favourable turn dramatically if the scaling matrix is slightly improved and a simple preconditioning technique is adopted: For naturally chosen
Since explicit ®nite dierence formulations directly compute the ¯ow variables at the new time level from the known initial conditions, implementing a standard multigrid
More speci®cally, the present paper describes how the GITT can be used to derive analytical solutions for solute transport problems in porous media with spatially and
Validation of SEWAB with ®eld data from the FIFE experiment proved that the turbulent sensible and latent heat ¯ux can quite well be reproduced by adapting the initial soil
For fBm media, this size dependence can be explained using an eective variance that increases with increasing size of the ¯ow system.. However, the magnitudes of the
9 illustrates the mesh evolution in this computation (we demonstrate only a quarter of meshes in this set): the upper grid is initially generated with 115 points and 160 elements;
Based on the analyses of these 28 streamflow time series and 13 artificially generated signals with known dynamics, no direct relationship between the nature of underlying
C onstructing diagrams to explain certain physiological concepts can be challeng- ing. There is a whole class of physiological topics, represented here by the neural generation
