Research Article
Influence of Hydrological Model Selection on Simulation of Moderate and Extreme Flow Events: A Case Study of the Blue Nile Basin
Table 1
Meteorological and hydrological stations.
| S. number | GHCN_ID | Station | Long. | Lat. | PM (%) |
| Rainfall |
| 1 | ET000063331 | Gondar | 37.42 | 12.55 | 0.0 | 2 | ET000063332 | Bahar Dar | 37.42 | 11.60 | 0.0 | 3 | ET000063333 | Combolcha | 39.73 | 11.12 | 0.3 | 4 | ET000063334 | Debre Marcos | 37.67 | 10.33 | 0.0 | 5 | ET000063402 | Jimma | 36.83 | 7.67 | 0.1 | 6 | ET000063403 | Gore | 35.53 | 8.15 | 0.6 | 7 | SU000062721 | Khartoum | 32.55 | 15.60 | 0.3 | 8 | SU000062752 | Gedaref | 35.40 | 14.03 | 0.0 | 9 | SU000062762 | Sennar | 33.62 | 13.55 | 0.8 | 10 | SU000062730 | Kassala | 36.40 | 15.47 | 0.9 | 11 | ET000063330 | Makale | 39.48 | 13.50 | 1.1 | 12 | ET000063450 | Addis Ababa-Bole | 38.75 | 9.03 | 0.5 | 13 | ET000063451 | Harar Meda | 38.95 | 8.73 | 0.6 | 14 | ET000063453 | Metehara | 39.90 | 8.87 | 0.7 |
| Flow |
| A | | Khartoum | 32.51 | 15.64 | 0.0 | B | | El Diem | 34.93 | 11.24 | 0.0 | C | | Ribb | 37.73 | 12 | 0.0 |
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: missing station ID; PM: percentage of missing records; long.: longitude [°]; lat.: latitude [°].
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