ANALISIS SUHU UDARA, KELEMBAPAN UDARA, DAN TEKANAN UDARA TERHADAP CURAH HUJAN (STUDY KASUS : KOTA SERANG)

Article Sidebar

PDF
Published: Jun 28, 2025
DOI: https://doi.org/10.67006/charmsains.v6i2.438
Keywords:
Rainfall, Partially, Simultaneously

Main Article Content

Mila Nuridhati
Universitas Sultan Ageng Tirtayasa
Yayat Ruhiat
Universitas Sultan Ageng Tirtayasa
Yudi Guntara
Universitas Sultan Ageng Tirtayasa

Abstract

This study aims to analyze the impact of air temperature, air humidity, and air pressure on rainfall, both individually and simultaneously. The method applied is multiple linear regression, with secondary data for 5 years from 2019 to 2023. The results  showed that air humidity, air pressure, and minimum air temperature have a positive influence on rainfall, while maximum air temperature has  a negative influence.  Simultaneously air humidity, air pressure, minimum temperature, and maximum temperature together have a significant effect on rainfall by 55,6%. However, artially, only the minimum air temperature has a significant effect, while the variables of maximum air temperature, air humidity, and air pressure do not show a significant effect.

Article Details

How to Cite
Mila Nuridhati, Ruhiat, Y., & Guntara, Y. (2025). ANALISIS SUHU UDARA, KELEMBAPAN UDARA, DAN TEKANAN UDARA TERHADAP CURAH HUJAN (STUDY KASUS : KOTA SERANG) . Charm Sains: Jurnal Pendidikan Fisika, 6(2), 96-101. https://doi.org/10.67006/charmsains.v6i2.438
Issue
Vol 6 No 2 (2025): JUNI
Section
Articles
Creative Commons License

This work is licensed under a Creative Commons Attribution 4.0 International License.

References

Al Azkia, W. M., Hitayuwana, N., Khusna, Z. A., & Widodo, E. (2019). Analisis temperature dan kelembaban terhadap curah hujan di Kabupaten Sleman Provinsi Daerah Istimewa Yogyakarta.
Amalia, M., & Faizin, F. (2023). Kota serang dalam angka 2023.
Hermawan, E., Soeparmo, S. H., & Kemlrah, A. (2006). Analisis stabilitas atmosfer pada lapisan troposfer atas dan stratosfer bawah di atas Kototabang menggunakan data Equatorial atmosphere radar (EAR), Boundary layer radar (BLR) dan Radiosonde. Jurnal Sains Dirgantara, 3(2), 112–130. http://jurnal.lapan.go.id/index.php/jurnal_sains/article/view/655
Pabalik, I., Ihsan, N., & Arsyad, M. (2015). Analisis Fenomena Perubahan Iklim dan Karakteristik Curah Hujan Ekstrim di Kota Makassar. Jurnal Sains Dan Pendidikan Fisika, 11(1), 88–92.
Pradipta, N. S., Sembiring, P., & Bangun, P. (2013). Analisis Pengaruh Curah Hujan di Kota Medan. Saintia Matematika, 1(5), 459–468.
Purwakinanti, R., Rusgiyono, A., & Prahutama, A. (2014). Aplikasi metode momen probabilitas terboboti untuk estimasi parameter distribusi pareto terampat pada data curah hujan. Jurnal Gaussian, 3(4), 821–830. https://doi.org/http://ejournal-s1.undip.ac.id/index.php/gaussian
Tabari, H. (2020). Climate change impact on flood and extreme precipitation increases with water availability. Scientific Reports, 10(1), 1–10. https://doi.org/10.1038/s41598-020-70816-2
Tresnaeni, S. D. (2020). Analisis Faktor Unsur Cuaca Yang Mempengaruhi Aktivitas Penerbangan Di Bandara Ahmad Yani Semarang Tahun 2018 Dengan Metode Principal Component Analysis. 1–77.
Tukidi. (2010). Karakter Curah Hujan Di Indonesia. Jurnal Geografi, 7(2), 136–145. http://journal.unnes.ac.id/nju/index.php/JG/article/view/84
Wati, S. E., Sebayang, D., & Sitepu, R. (2013). Perbandingan Metode Fuzzzy Dengan Regresi LInier Berganda Dalam Peramlan Jumlah Produksi. Saintia Matematika, 1(3), 273–284.