Research Article
Drought Analysis in East Nusa Tenggara (Indonesia) Using Regional Frequency Analysis
Table 3
Estimated L-moment ratio, discordancy, and heterogeneity statistic for the daily rainfall average in the five homogeneous regions.
| Region | Station (Di) | L − | L − CsR | L − CkR | Dcritical | H1 |
| 1 | Komodo | 0.539 | 0.424 | 0.214 | — | — | 2 | Frans Sales Lega | 0.519 | 0.350 | 0.155 | — | — | 3 | Fransiskus Xaverius (1), Gewayantana (1), Mali (1) | 0.570 | 0.455 | 0.233 | 3 | 0.63 | 4 | Umbu Mehang Kunda (1), Tardamu (1) | 0.557 | 0.432 | 0.209 | 3 | 0.32 | 5 | Kupang (1), Eltari (1) | 0.568 | 0.442 | 0.225 | 3 | 1.83 |
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