2020
DOI: 10.22146/jcef.57125
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Application of TRMM in the Hydrological Analysis of Upper Bengawan Solo River Basin

Abstract: Rainfall is a major water resource with a significant role in terms of growth, environment concerns, and sustainability. Several human activities demand adequate water supply for drinking, agriculture, domestic, and commercial consumption. The accuracy of any hydrologic study depends heavily on the availability of good-quality precipitation estimates. Most countries are unable to provide sufficient climatic data, including rainfall and observed discharge statistics. This scarcity is a huge obstacle in conducti… Show more

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Cited by 9 publications
(8 citation statements)
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“…Stage 1: Spatially plotting all TRMM grids and observation stations to be used in the study area (ii). Stage 2, selecting TRMM grids based on the correlation and RMSE analysis of TRMM grids to observation stations, with the criteria that the selected TRMM grid for validation must correlate (r) to the observation station ≥ 0.6 (Senjaya, 2020) and RMSE ≤ 130 mm (Soeryamassoeka, 2020). (iii).…”
Section: Analysis Of Trmm Satellite Rainfallmentioning
confidence: 99%
“…Stage 1: Spatially plotting all TRMM grids and observation stations to be used in the study area (ii). Stage 2, selecting TRMM grids based on the correlation and RMSE analysis of TRMM grids to observation stations, with the criteria that the selected TRMM grid for validation must correlate (r) to the observation station ≥ 0.6 (Senjaya, 2020) and RMSE ≤ 130 mm (Soeryamassoeka, 2020). (iii).…”
Section: Analysis Of Trmm Satellite Rainfallmentioning
confidence: 99%
“…Nevertheless, such satellite-derived data require proper corrections before using them for computations because they are affected by a lot of uncertainty, such as sun radiation, temperature, cloud cover, etc. (Senjaya et al, 2020). In our study, the regional rainfall values for the Katulampa watershed were computed using the Thiessen polygon method, as seen in Figure 3.…”
Section: Case Studymentioning
confidence: 99%
“…Model HBV-96 membagi lapisan tanah menjadi tiga dan satu channel routing berdasarkan respon tanah terhadap hujan. Empat lapisan tersebut diantaranya yaitu: X1 (Soil Moisture Storage), X2 (Upper Storage), X3 (Lower Storage/Ground Water) dan X4 (aliran air sungai) (Senjaya et al, 2020). Pada Model HBV96, parameter model yang mempengaruhi aliran dasar adalah kecepatan air mengalir ke bawah karena proses perkolasi alami, koefisien daya untuk recharge dan perkolasi, tinggi kelembaban tanah aktual, koefisien untuk aliran air tanah, dan kapasitas penyimpanan kelembaban tanah maksimum.…”
Section: ) Model Hbv-96unclassified