### Table 3 contains the projection errors and the errors introduced in the pressure and velocity eld by the upscaling methods discussed above. Clearly,

in Global upscaling of permeability in heterogeneous reservoirs; The output least squares (OLS) method.

1998

Cited by 5

### Table 5: Numerical results obtained in Example 2; Relative error in the pressure and velocity eld.

in Global upscaling of permeability in heterogeneous reservoirs; The output least squares (OLS) method.

1998

Cited by 5

### Table 7: Numerical results obtained in Example 3; Relative error in the pressure and velocity eld.

in Global upscaling of permeability in heterogeneous reservoirs; The output least squares (OLS) method.

1998

Cited by 5

### Table 1. Critical dynamo numbers Ccrit , growth rates of magnetic energy and drift velocities !m of the magnetic eld modes m = 0, 1, 2 in a model with axially symmetric velocity eld

### Table 1. Critical dynamo numbers Ccrit , growth rates of magnetic energy and drift velocities !m of the magnetic eld modes m = 0, 1, 2 in a model with axially symmetric velocity eld.

### Table 5.2. sQMR iterations for different velocity elds and xed regularization parameter a a165 1.

2005

### Tables 5.1 sQMR iterations for different velocity elds and xed regularization pa- rameter a a3 10a4 4. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 34

2005

### Table 5.1. sQMR iterations for different velocity elds and xed regularization parameter a a165 10a166 4.

2005

### Table 5.7. sQMR iterations for different velocity elds and xed regularization parameter a a165 10a166 4.

2005

### Table 1: The actual velocities, the estimated velocities, the error ratios and the number of pixels of the three major motion elds in Fig. 8.

"... In PAGE 8: ... There are 33 cluster centres detected in the feature space, where di erent classes are shown as di erent grey levels in the segmentation map. Table1 shows the actual velocities ~uactual, the estimated velocities ~uestimated, the error ratios and the number of pixels of the three major regions with distinct group velocities, which correspond to the two disks and the background. The error ratio is de ned as k~uactual ? ~uestimatedk k~uactualk : (13) Both disks are classi ed as homogeneous optical ow elds, and the estimated velocities ap- proximate the actual velocities (error ratio 10?3).... ..."