Four different layering configurations were investigated, including a homogeneous case (case H), and three different layered cases where a low permeability layer was set at the top of the aquifer (case LH), at the middle part of the aquifer as interlayer (case HLH), and at the lower part of the aquifer (case HL).
The approach for clustering based on example similarity, presented in the previous section for a single-layer case, can be easily extended to clustering in a multi-layer case.
In a multi-layer case, two cells are closest when placed directly one over the other, i.e., on the same location but on separate layers.
To obtain the mapping in an n+1 layer case, we rewrite the system Eq. (3) as where [ B], [ C], [ D], [ E], [ F], [ G] represent here submatrices of the complete BEM matrix corresponding to the uninteresting parameters.
The domain area is 16 times larger than in sections 'Convective adjustment in unstable layer (case A)' and 'Microscale eddies induced by turbulent thermal flux (case B)'. Figure 13 shows time-height cross sections of area-mean θ ′ w ′ ¯, q ′ w ′ ¯, and u ′ w ′ ¯ for large-domain experiments of cases A10 and B3 under the condition U Z = 0 m · s 1 · km 1.
To confirm the presence of microscale eddies in the large model domain, domain size (5 × 5 km) in sections 'Convective adjustment in unstable layer (case A)' and 'Microscale eddies induced by turbulent thermal flux (case B)' is extended by a factor of four (to 20 × 20 km) in the large-domain experiment (section 'Sensitivity of microscale eddies to model domain size').
In a case layered with ethnicity, history and politics, Mr. Gonzales and other heirs are asking for reparations, saying the government cheated their forebears, in some cases paying them nothing, even as nearby Anglo landowners received far more money for their property.
For Newmont, five of whose employees were jailed in Jakarta last year, the trial has been a major irritant, not least because of what it sees as the Indonesian legal system's arbitrariness, as well as its potential unpreparedness for a case layered with environmental science.
From a two-layer reference solution, an explicit solution for the multi-layer case is derived.
Focusing on the two-layer case, we present a numerical improvement that locally avoids the loss of hyperbolicity.
The convective adjustments are simulated in case A (A02 to A30, section 'Convective adjustment in unstable layer (case A)').
