Table 10.
Similarity in extracted values and isoline zones for the different parameters from various datasets in comparison to the T50A dataset
Sl. No. | Dataset | Difference class from T50A values | Average elevation | Relative relief | Slope | Drainage density | Averaged totals | Remarks | ||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
Difference class range (m) | % Basin area | Total % | Difference class range (m) | % Basin area | Total % | Difference class range (degrees) | % Basin area | Total % | Difference class range (km / sqkm) | % Basin area | Total % | |||||
1 | A30 | Immediate greater | −100 to 0 | 47.19 | 85.42 | −250 to 0 | 40.06 | 99.26 | −10 to 0 | 80.85 | 94.23 | −2 to 0 | 11.55 | 50.20 | 82.28 | Very high match |
Immediate lesser | 0 to 100 | 38.23 | 0 to 250 | 59.20 | 0 to 10 | 13.38 | 0 to 2 | 38.65 | ||||||||
2 | A90 | Immediate greater | −500 to 0 | 25.60 | 52.87 | −250 to 0 | 38.53 | 72.24 | −10 to 0 | 38.65 | 58.52 | −2 to 0 | 32.01 | 70.78 | 63.60 | Low match |
Immediate lesser | 0 to 500 | 27.27 | 0 to 250 | 33.71 | 0 to 10 | 19.87 | 0 to 2 | 38.77 | ||||||||
3 | C30 | Immediate greater | −100 to 0 | 50.75 | 65.55 | −250 to 0 | 53.80 | 93.97 | −10 to 0 | 70.93 | 82.41 | −2 to 0 | 9.22 | 47.82 | 72.44 | Moderate match |
Immediate lesser | 0 to 100 | 14.80 | 0 to 250 | 40.17 | 0 to 10 | 11.48 | 0 to 2 | 38.60 | ||||||||
4 | C90 | Immediate greater | −500 to 0 | 27.04 | 54.62 | −250 to 0 | 42.15 | 69.62 | −10 to 0 | 37.41 | 50.80 | −2 to 0 | 32.32 | 71.20 | 61.56 | Low match |
Immediate lesser | 0 to 500 | 27.58 | 0 to 250 | 27.47 | 0 to 10 | 13.39 | 0 to 2 | 38.88 | ||||||||
5 | S90 | Immediate greater | −100 to 0 | 48.74 | 86.23 | −250 to 0 | 62.39 | 98.94 | −10 to 0 | 80.68 | 87.65 | −2 to 0 | 39.68 | 76.85 | 87.42 | Very high match |
Immediate lesser | 0 to 100 | 37.49 | 0 to 250 | 36.55 | 0 to 10 | 6.97 | 0 to 2 | 37.17 | ||||||||
6 | T50D | Immediate greater | −100 to 0 | 60.61 | 94.12 | −250 to 0 | 94.88 | 99.86 | −10 to 0 | 82.81 | 84.76 | −2 to 0 | 48.77 | 78.48 | 89.31 | Highest match |
Immediate lesser | 0 to 100 | 33.51 | 0 to 250 | 4.98 | 0 to 10 | 1.95 | 0 to 2 | 29.71 | ||||||||
7 | T250A | Immediate greater | −500 to 0 | 46.95 | 74.96 | −250 to 0 | 30.60 | 47.43 | −10 to 0 | 31.43 | 52.04 | −2 to 0 | 48.55 | 71.57 | 61.50 | Lowest match |
Immediate lesser | 0 to 500 | 28.01 | 0 to 250 | 16.83 | 0 to 10 | 20.61 | 0 to 2 | 23.02 | ||||||||
8 | T250D | Immediate greater | −500 to 0 | 47.16 | 74.93 | −250 to 0 | 38.64 | 58.79 | −10 to 0 | 29.67 | 42.83 | −2 to 0 | 41.85 | 79.06 | 63.90 | Low match |
Immediate lesser | 0 to 500 | 27.77 | 0 to 250 | 20.15 | 0 to 10 | 13.16 | 0 to 2 | 37.21 |
Differences for each dataset are computed parameter-wise by subtracting from the corresponding values of that same parameter in the T50A database for each of the 1154 grids and isopleth classes are then demarcated on basis of this difference. Thus the immediate greater class (where T50A values are higher) and immediate lesser class (where T50A values are lower) together show areas which are more closely approximate to the values of the surveyed T50A database. If these two ranges combined, cover a greater proportion of the basin area, it implies then that that dataset matches well with the surveyed topographical map database, in terms of the parameters extracted and their ensuing isopleth zones. Perfect matching would give a narrow difference class range around zero covering the total basin area