Model Pendugaan Kekeringan Dengan Menggunakan Konsep Neraca Air Thornthwaite & Mather (Studi Kasus Di Sub Das Seluna)

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Handoko, Ungul; Boer, Rizaldi; Soepri, Wahyoe; Faqih, Akhmad; Zulti, Fifia, 2018, "Model Pendugaan Kekeringan Dengan Menggunakan Konsep Neraca Air Thornthwaite & Mather (Studi Kasus Di Sub Das Seluna)", https://hdl.handle.net/20.500.12690/RIN/DFUKDX, RIN Dataverse, V1

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Description

Studi model pendugaan kekeringan di Sub DAS Seluna dengan menggunakan metode neraca air Thornthwaite & Mather telah dilakukan. Data yang digunakan untuk studi pemodelan kekeringan ini berasal dari data sekunder iklim, jenis tanah dan luas kekeringan aktual di daerah penelitian. Hasil studi menunjukkan bahwa kekeringan mulai terjadi pada saat kondisi air tersedia turun sampai dengan 30 persenKL. Kejadian kekeringan di Sub DAS Seluna rata-rata terjadi pada bulan Agustus-Oktober dan sebagian besar saat kondisi air kurang dari 30 persen KL, dengan daerah-daerah yang mengalami kekeringan Blora, Pati, Kudus,Grobogan dan Rembang, serta sebagian kecil Boyolali dan Sragen. Pendekatan analisis model kekeringan mampu menggambarkan sebaran wilayah kekeringan di daerah penelitian dengan cukup baik. Hal ini ditandai nilai korelasi antara kekeringan model dan kekeringan aktual yang kuat (0.61).Kata Kunci : Kekeringan, Thornthwaite&Mather, Sub DAS Seluna

Prosiding Seminar Nasional Limnologi VII 2014

(2014)

Subject

Earth and Environmental Sciences


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Citation Metadata

Dataset Persistent ID	hdl:20.500.12690/RIN/DFUKDX
Publication Date	2018-03-25
Title	Model Pendugaan Kekeringan Dengan Menggunakan Konsep Neraca Air Thornthwaite & Mather (Studi Kasus Di Sub Das Seluna)
Author	Handoko, Ungul (Pusat Penelitian Limnologi) Boer, Rizaldi (Pusat Penelitian Limnologi) Soepri, Wahyoe (Pusat Penelitian Limnologi) Faqih, Akhmad (Pusat Penelitian Limnologi) Zulti, Fifia (Pusat Penelitian Limnologi)
Contact	Use email button above to contact. Zulti, Fifia (Pusat Penelitian Limnologi)
Description	Studi model pendugaan kekeringan di Sub DAS Seluna dengan menggunakan metode neraca air Thornthwaite & Mather telah dilakukan. Data yang digunakan untuk studi pemodelan kekeringan ini berasal dari data sekunder iklim, jenis tanah dan luas kekeringan aktual di daerah penelitian. Hasil studi menunjukkan bahwa kekeringan mulai terjadi pada saat kondisi air tersedia turun sampai dengan 30 persenKL. Kejadian kekeringan di Sub DAS Seluna rata-rata terjadi pada bulan Agustus-Oktober dan sebagian besar saat kondisi air kurang dari 30 persen KL, dengan daerah-daerah yang mengalami kekeringan Blora, Pati, Kudus,Grobogan dan Rembang, serta sebagian kecil Boyolali dan Sragen. Pendekatan analisis model kekeringan mampu menggambarkan sebaran wilayah kekeringan di daerah penelitian dengan cukup baik. Hal ini ditandai nilai korelasi antara kekeringan model dan kekeringan aktual yang kuat (0.61).Kata Kunci : Kekeringan, Thornthwaite&Mather, Sub DAS Seluna Prosiding Seminar Nasional Limnologi VII 2014 (2014)
Subject	Earth and Environmental Sciences
Depositor	Wulandari, Desi
Deposit Date	2018-03-25

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