Comparison of Bright Band Radar from GPM and MRR Observation in West Sumatera
The Bright band (BB) observation can be used as an indication of the melting layer height. Measurement of BB from Normal Scan (NS) on Global Precipitation Measurement (GPM) had been compared with Micro Rain Radar (MRR), which is installed in Kototabang, West Sumatera (0.23o S; 100.32oE; 865 m above...
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| Format: | Article |
| Language: | English |
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Universitas Negeri Surabaya
2021-10-01
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| Series: | Jurnal Penelitian Fisika dan Aplikasinya |
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| Online Access: | https://journal.unesa.ac.id/index.php/jpfa/article/view/9952 |
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| author | Ravidho Ramadhan Marzuki Marzuki Mutya Vonnisa Harmadi Harmadi Hiroyuki Hashiguchi Toyoshi Shimomai |
| author_facet | Ravidho Ramadhan Marzuki Marzuki Mutya Vonnisa Harmadi Harmadi Hiroyuki Hashiguchi Toyoshi Shimomai |
| author_sort | Ravidho Ramadhan |
| collection | DOAJ |
| description | The Bright band (BB) observation can be used as an indication of the melting layer height. Measurement of BB from Normal Scan (NS) on Global Precipitation Measurement (GPM) had been compared with Micro Rain Radar (MRR), which is installed in Kototabang, West Sumatera (0.23o S; 100.32oE; 865 m above sea level). The GPM data were collected from December 2014 to June 2018 and compared with MRR observation from January 2012 to August 2016. The BB values from these instruments were also compared with the values recommended by the International Telecommunication Union Recommendation (ITU-R) P.839. The BB from GPM and MRR showed slightly diurnal and seasonal variations. BB observations from GPM and MRR show good agreement with slightly difference in diurnal and seasonal variations. BB observations are more similar when the intensity of solar radiation is lower, i.e. at night (18.00-24.00 LT) until early morning (00.00-06.00 LT). Furthermore, MRR showed a slight bimodal pattern in the seasonal variation while GPM did not. Thus, the seasonal variation in observation of both instrument is different. The largest different from the seasonal variation was observed in the summer season (June-August(JJA)). The mean BB of the two instruments is lower than the Freezing Height Level (FHL) value calculated from the ITU-R model. However, many BB from the two instruments (>36 %) has a BB altitude higher than FHL. Thus, the constant assumption of FHL in West Sumatera for the rain attenuation estimation of microwaves may not be appropriate. |
| first_indexed | 2024-04-09T23:40:05Z |
| format | Article |
| id | doaj.art-05c58398cc2044af81653eb01848f8a6 |
| institution | Directory Open Access Journal |
| issn | 2087-9946 |
| language | English |
| last_indexed | 2024-04-09T23:40:05Z |
| publishDate | 2021-10-01 |
| publisher | Universitas Negeri Surabaya |
| record_format | Article |
| series | Jurnal Penelitian Fisika dan Aplikasinya |
| spelling | doaj.art-05c58398cc2044af81653eb01848f8a62023-03-19T03:27:39ZengUniversitas Negeri SurabayaJurnal Penelitian Fisika dan Aplikasinya2087-99462021-10-01111506210.26740/jpfa.v11n1.p50-6216455Comparison of Bright Band Radar from GPM and MRR Observation in West SumateraRavidho Ramadhan0Marzuki Marzuki1Mutya Vonnisa2Harmadi Harmadi3Hiroyuki Hashiguchi4Toyoshi Shimomai5Universitas AndalasUniversitas AndalasUniversitas AndalasUniversitas AndalasKyoto UniversityShimane UniversityThe Bright band (BB) observation can be used as an indication of the melting layer height. Measurement of BB from Normal Scan (NS) on Global Precipitation Measurement (GPM) had been compared with Micro Rain Radar (MRR), which is installed in Kototabang, West Sumatera (0.23o S; 100.32oE; 865 m above sea level). The GPM data were collected from December 2014 to June 2018 and compared with MRR observation from January 2012 to August 2016. The BB values from these instruments were also compared with the values recommended by the International Telecommunication Union Recommendation (ITU-R) P.839. The BB from GPM and MRR showed slightly diurnal and seasonal variations. BB observations from GPM and MRR show good agreement with slightly difference in diurnal and seasonal variations. BB observations are more similar when the intensity of solar radiation is lower, i.e. at night (18.00-24.00 LT) until early morning (00.00-06.00 LT). Furthermore, MRR showed a slight bimodal pattern in the seasonal variation while GPM did not. Thus, the seasonal variation in observation of both instrument is different. The largest different from the seasonal variation was observed in the summer season (June-August(JJA)). The mean BB of the two instruments is lower than the Freezing Height Level (FHL) value calculated from the ITU-R model. However, many BB from the two instruments (>36 %) has a BB altitude higher than FHL. Thus, the constant assumption of FHL in West Sumatera for the rain attenuation estimation of microwaves may not be appropriate.https://journal.unesa.ac.id/index.php/jpfa/article/view/9952bright bandgpmmrrdiurnal variationseasonal variation. |
| spellingShingle | Ravidho Ramadhan Marzuki Marzuki Mutya Vonnisa Harmadi Harmadi Hiroyuki Hashiguchi Toyoshi Shimomai Comparison of Bright Band Radar from GPM and MRR Observation in West Sumatera Jurnal Penelitian Fisika dan Aplikasinya bright band gpm mrr diurnal variation seasonal variation. |
| title | Comparison of Bright Band Radar from GPM and MRR Observation in West Sumatera |
| title_full | Comparison of Bright Band Radar from GPM and MRR Observation in West Sumatera |
| title_fullStr | Comparison of Bright Band Radar from GPM and MRR Observation in West Sumatera |
| title_full_unstemmed | Comparison of Bright Band Radar from GPM and MRR Observation in West Sumatera |
| title_short | Comparison of Bright Band Radar from GPM and MRR Observation in West Sumatera |
| title_sort | comparison of bright band radar from gpm and mrr observation in west sumatera |
| topic | bright band gpm mrr diurnal variation seasonal variation. |
| url | https://journal.unesa.ac.id/index.php/jpfa/article/view/9952 |
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