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All Journal POSITRON Jurnal Penelitian Fisika dan Aplikasinya (JPFA) TELKOMNIKA (Telecommunication Computing Electronics and Control) Jurnal Fisika Unand Emerging Science Journal Jurnal Penelitian Pendidikan IPA (JPPIPA) Logista: Jurnal Ilmiah Pengabdian Kepada Masyarakat Jurnal Ilmu Fisika MONSU'ANI TANO Jurnal Pengabdian Masyarakat Riyadhoh : Jurnal Pendidikan Olahraga BERNAS: Jurnal Pengabdian Kepada Masyarakat Warta Pengabdian Andalas: Jurnal Ilmiah Pengembangan Dan Penerapan Ipteks
Marzuki Marzuki
Department Of Physics, Faculty Of Mathematics And Natural Sciences, Universitas Andalas, Padang 2516, West Sumatra, Indonesia
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Journal : Emerging Science Journal

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Vertical Characteristics of Raindrops Size Distribution over Sumatra Region from Global Precipitation Measurement Observation Ravidho Ramadhan; . Marzuki; . Harmadi
Emerging Science Journal Vol 5, No 3 (2021): June
Publisher : Ital Publication

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.28991/esj-2021-01274

Abstract

The climatology of the vertical profile of raindrops size distribution (DSD) over Sumatra Region (10° S – 10° N, 90° E – 110° E) has been investigated using Global Precipitation Measurement (GPM) level 2 data from January 2015 to June 2018. DSD's vertical profile was observed through a vertical profile of corrected radar reflectivity (Ze) and two parameters of normalized gamma DSD, i.e., mass-weight mean diameter (Dm) and total drops concentration (Nw). Land-ocean contrast and rain type dependence of DSD over Sumatra were clearly observed. The values of Dm and Nw were larger in the land than in the ocean. Negative and positive gradients of Dm toward the surface were dominant during stratiform and convective rains, respectively, consistent with the Z gradient. Moreover, the negative gradient of stratiform rain in the ocean is larger than in land. Thus, the depletion of large drops is dominant over the ocean, which is due to the break-up process that can be observed from the increase of Nw. Raindrop growth of convective rains is more robust over the ocean than land that can be seen from a larger value of Dmgradient. The BB strength is slightly larger over land and coastal region than over the ocean, indicating that the riming process is more dominant over land and coastal regions than the ocean. Doi: 10.28991/esj-2021-01274 Full Text: PDF
Retrieval of Vertical Structure of Raindrop Size Distribution from Equatorial Atmosphere Radar and Boundary Layer Radar Mutya Vonnisa; Toyoshi Shimomai; Hiroyuki Hashiguchi; Marzuki Marzuki
Emerging Science Journal Vol 6, No 3 (2022): June
Publisher : Ital Publication

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.28991/ESJ-2022-06-03-02

Abstract

This work develops an algorithm to retrieve the vertical structure of the raindrop size distribution (DSD) of rain from simultaneous observations of 47 MHz Equatorial Atmosphere Radar (EAR) and 1.3 GHz Boundary Layer Radar (BLR) at Koto Tabang, West Sumatra, Indonesia (0.20°S, 100.32°E, 865 m above sea level). EAR is sensitive to the detection of turbulence, and BLR is susceptible to identifying precipitation echo. The EAR Doppler spectrum broadening effects due to turbulence and finite radar beam width were reduced using the convolution process. The Gaussian function was used to model the turbulence Doppler spectrum. A non-linear least-squares fitting method was applied to retrieve DSD parameters. Subsequently, the equations to estimate DSD using this dual-frequency algorithm assume the gamma DSD model to retrieve the distribution from the Doppler spectrum of precipitation echo. The precipitation events on April 23, 2004 on the Coupling Processes in the Equatorial Atmosphere (CPEA-I) project have been analyzed. Results show that the precipitation spectrum obtained using the dual-frequency method is higher, more precise, and well-fitted than the single-frequency method, meaning the dual-frequency method has great potential to be used in observing the microphysical process and remote sensing application analysis of DSD in Indonesia, particularly at Koto Tabang. The analyses show various microphysical processes that occur in the rain, such as coalescence, evaporation, break-up, and condensation. Furthermore, for the purpose of easier remote sensing application analysis of profile DSD characteristics, we use a DSD ΔΖMP parameter. ΔΖMP is a rain rate insensitive DSD parameter representing mean drop size. The trend of ΔZMP is not totally uniform with regards to rain rate and reflectivity factors, with ΔZMP higher in the first half of the event and becoming lower toward the end. This suggests that we have to use different Z-R relations within the event. Doi: 10.28991/ESJ-2022-06-03-02 Full Text: PDF
Co-Authors -, Renanto Adi Susilo Afdal, Afdal Afdhal Muttaqin Afrizal Afrizal Ahmad Fauzi Pohan Ahmad Rizqy Shubri Ahmad Zul Amal Zaini Ardian Putra Arif Budiman Arif Ismul Hadi Astuti Astuti Astuti Astuti Astuti Aulya Rahayu Aulya Rahayu Aulya Rahayu, Aulya Awaluddin Awaluddin Awaluddin Awaluddin Ayu Putri Ningsih Ayu Putri Ningsih Bella Deswanti Bunga Aprilia Dahyunir Dahlan Dea Kurnia Harysandi Dea Kurnia Harysandi Deasy Arisa Dedi Mardiansyah Dian Fitriyani Dinda Maulani Adfy Dwi Pujiastuti Dwi Puryanti Dwianda, Rany Audia Elfira Saufina Elfira Saufina Elvaswer Elvaswer Fadilla Monica Fadli Nauval Faridah Salma Feri Helmi Basri Feriska Handayani Irka, Feriska Handayani Fery Kurnia Sandi Gina Felita Harmadi Harmadi Harysandi, Dea Kurnia Helmi Yusnaini Helmi Yusnaini Helmi Yusnaini Helmi Yusnaini Hiroyuki Hashiguchi Hiroyuki Hashiguchi Hiroyuki Hashiguchi Hiroyuki Hashiguchi Hiroyuki Hashiguchi Hiroyuki Hashiguchi Hiroyuki Hashiguchi Hiroyuki Hashiguchi Hiroyuki Hashiguchi Hiroyuki Hashiguchi, Hiroyuki Ikhwan Fikri Maulidan Imam Taufik Imam Taufiq Indah Rahayu Iqbal Ramadhan Irza Utami L. Luini Lismalini Lismalini Lismalini, Lismalini Lisna Meylani Lusi Fitrian Sani Lusi Fitrian Sani Lusi Fitrian Sani, Lusi Fitrian Melly Angglena Meqorry Yusfi Meri Yoseva Mohammad Ali Shafii Mora Mora Mora Mora Mora Muchtia Rahma Muchtia Rahma, Muchtia Muhammad Arif Muhammad Kahfi Muharsyah, Robi Muldarisnur, Mulda Mutya Vonnisa Muzirwan Muzirwan Naela Amalia Zulfa Nauval, Fadli Nina Nina Nini Firmawati Nor Azlan Mohd Aris Novianti Indrastuti Nugroho, Susilo Nur Fadillah Nurdin Nurdin Nurul Hasanah Poltak Sandro Rumahorbo Poltak Sandro Rumahorbo, Poltak Sandro Puja Kasmailen Putri Rahmad Rasyid Rahmad Rasyid Rahmat Rasyid Ramacos Fardela Ramadani Safitri Ramadani Safitri Ramadhan, Ravidho Rani Delvihardini Rany Audia Dwianda Ravidho Ramadhan Ravidho Ramadhan Ravidho Ramadhan Ravidho Ramadhan Ravidho Ramadhan Ravidho Ramadhan Rifa Lihayati Rini Oktaviani Rio Chandra Rio Chandra, Rio Robi Muharsyah Salma, Faridah Selly Tridaiana Shimomai, Toyoshi Sholihun, Sholihun Silvia Wahyuni Solly Aryza Sri Hamdiyessi Sri Handani Sri Herlinda Sri Mai Dewi Sri Oktamuliani Sri Wahyuni Sri Wahyuni Sucy Lestari Wirma Sugeng Nugroho Suryanti, Krisna Suryanto, Wiwit Syarifatul Ulfah Toyoshi Shimomai Toyoshi Shimomai Toyoshi Shimomai Toyoshi Shimomai Toyoshi Shimomai Toyoshi Shimomai Trengginas Eka Putra Sutantyo Triana Vitri Triana Vitri, Triana Ulfa Azmi Usna, Sri Rahayu Alfitri Vira Friska Vira Friska Vira Friska Wendi Harjupa Wildian Wildian Wira Indrayani Yudi Saputra Zul Ikram Zulfi Zulfi Zulfi