Raindrop Size Distribution and Wind-Driven Rain Specific Attenuation: CCDF-Based Analysis at 18 and 38 GHz in Tropical Country
DOI:
https://doi.org/10.31436/iiumej.v27i2.4008Keywords:
5G, 6G, Rain Attenuation, DSD, specific attenuation, mm-waveAbstract
Seasonal monsoons, frequency dependence, and wind effects were investigated for rain-specific attenuation at millimeter-wave (mm-wave) frequencies in a tropical environment. Using one-minute RD-69 DSD data and matched wind observations, CCDFs of specific attenuation were evaluated at 18 and 38 GHz for three monsoon phases (SW, NE, IM) and four wind-direction sectors under unconstrained and constrained winds (9–11 m/s). The CCDF results show clear seasonal variability, with the SW monsoon producing the strongest attenuation and the largest mismatch from ITU-R P.838-3, particularly at 38 GHz. Error statistics show that the maximum deviation occurs in the SW 270°–360° sector, with an RMSE of 1.550 dB/km and a positive bias, confirming ITU-R underestimation. Meanwhile, the NE monsoon exhibits smaller overall deviations (worst-case RMSE below about 0.6 dB/km at 38 GHz). The IM period exhibits mixed behavior, where wind direction can shift the deviation between under- and overestimation under constrained winds. Exceedance levels of 0.01% and 0.001% were emphasized as design-relevant extremes, corresponding to approximately 52.6 min/year and 5.26 min/year, respectively, under one-minute sampling. Overall, the results indicate that ITU-R P.838-3 accuracy in tropical conditions depends on monsoon phase and wind direction, supporting monsoon-aware, direction-sensitive fade-margin planning and link-orientation considerations for robust 5G/6G terrestrial mm-wave systems.
ABSTRAK: Monsun bermusim, kebergantungan frekuensi, dan kesan angin telah dikaji terhadap pelemahan spesifik hujan pada frekuensi gelombang milimeter (mm-wave) dalam persekitaran tropika. Menggunakan data DSD RD-69 beresolusi satu minit dan melalui pemerhatian padanan angin, pelemahan CCDF spesifik dinilai pada 18 dan 38 GHz untuk tiga fasa monsun (SW, NE, IM) dan empat sektor arah angin di bawah angin tidak terkekang serta angin terkekang (9–11 m/s). Penyimpangan terbesar daripada ITU-R P.838-3 berlaku pada 38 GHz, khususnya semasa monsun barat daya (SW), apabila sektor 270°–360° di bawah angin tidak terkekang menunjukkan RMSE = 1.550 dB/km dan bias = +1.193 dB/km, menandakan ITU-R bernilai lebih rendah; di bawah angin terkekang, penyimpangan kekal tinggi (RMSE = 1.383 dB/km). Tempoh peralihan (IM) juga menunjukkan kebergantungan pada sektor angin terkekang, dengan RMSE = 1.212 dB/km dan bias = +0.936 dB/km pada 38 GHz, manakala monsun timur laut (NE) menunjukkan penyimpangan lebih kecil (RMSE terburuk adalah kurang daripada kira-kira 0.6 dB/km pada 38 GHz di bawah angin tidak terkekang). Tahap kebarangkalian lebihan 0.01% dan 0.001% ditekankan sebagai ekstrem yang relevan bagi reka bentuk, bersamaan kira-kira 52.6 min/tahun dan 5.26 min/tahun, masing-masing, pada pensampelan satu minit. Secara keseluruhan, dapatan kajian menunjukkan ketepatan ITU-R P.838-3 dalam keadaan tropika bergantung pada fasa monsun dan arah angin, sekaligus menyokong perancangan margin-pudaran yang peka monsun dan peka arah angin serta menimbang orientasi pautan untuk sistem gelombang-mm 5G/6G terestrial yang lebih berdaya tahan.
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