Claim Missing Document
Check
Articles

Found 3 Documents
Search
Journal : Agromet

ANALISIS PERUBAHAN IKLIM LOKAL DAN DEBIT SUNGAI DI DAS CIDANAUANALYSIS OF LOCAL CLIMATE CHANGE AND DISCHARGE IN CIDANAU WATERSHED Fadli Irsyad; Satyanto Krido Saptomo; Budi Indra Setiawan
Agromet Vol. 25 No. 1 (2011): JUNE 2011
Publisher : PERHIMPI (Indonesian Association of Agricultural Meteorology)

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (737.29 KB) | DOI: 10.29244/j.agromet.25.1.17-23

Abstract

Climate change causes uncertainty in water availability. The change may include annual rainfall, evapotranspiration and the shift of rainy and dry seasons, thus, it affects hydrological response in the region. Water demand will increase over time with population, industrial and business growth but the water availability has not been ascertained to sustainably satisfy those needs.  Cidanau Watershed has wetland ecosystem so-called the Rawa Danau (Caldera), with an area of around 2,500 ha. This watershed receives average annual rainfall around 2,500 mm. Climate change especially the local climate in the region of Cidanau was analyzed to illustrate how the relationship with Cidanau river discharge. It is expected that climate change does not affect the water availability in the watershed. In this study, the analysis of local climate change and its impact on the availability of water resources on Cidanau Watershed was based on climate trends, water balance analysis, and estimation of  discharge of Cidanau Watershed. This research was carried out using climate data and discharge from 1996 until 2010. The results showed that climate variables have changed from 1996 to 2010. This change mainly occurred in temperature, annual rainfall, and evapotranspiration. Based on the analysis, the discharge of Cidanau Watershed will decrease due to changes in rainfall and evapotranspiration. The estimated minimum river discharge of Cidanau Watershed ranges from 0.5 to 1 m3/s until 2050.
PENDUGAAN FLUKS PANAS DAN EVAPOTRANSPIRASI DENGAN JARINGAN SYARAF TIRUANHEAT FLUX AND EVAPOTRANSPIRATION ESTIMATION USING ARTIFICIAL NEURAL NETWORK Satyanto Krido Saptomo
Agromet Vol. 25 No. 1 (2011): JUNE 2011
Publisher : PERHIMPI (Indonesian Association of Agricultural Meteorology)

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (736.47 KB) | DOI: 10.29244/j.agromet.25.1.24-28

Abstract

Artificial neural network (ANN) approach was used to model energy dissipation process into sensible heat and latent heat (evapotranspiration) fluxes. The ANN model has 5 inputs which are leaf temperature Tl, air temperature Ta, net radiation Rn, wind speed uc and actual vapor pressure ea. Adjustment of ANN was conducted using back propagation technique, employing measurement data of input and output parameters of the ANN. The estimation results using the adjusted ANN shows its capability in resembling the heat dissipation process by giving outputs of sensible and latent heat fluxes closed to its respective measurement values as the measured input values are given.  The ANN structure presented in this paper suits for modeling similar process over vegetated surfaces, but the adjusted parameters are unique. Therefore observation data set for each different vegetation and adjustment of ANN are required.
Penentuan Awal dan Durasi Musim Kemarau Menggunakan Fungsi Polynomial dengan Aplikasi Visual Basic for Applications (VBA) Fadli Irsyad; Satyanto Krido Saptomo; Budi Indra Setiawan
Agromet Vol. 28 No. 1 (2014)
Publisher : PERHIMPI (Indonesian Association of Agricultural Meteorology)

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (497.975 KB) | DOI: 10.29244/j.agromet.28.1.40-46

Abstract

Forecasting the occurrence of the onset of dry season and its length is important in determining the availability of water for irrigation, domestic and industrial uses. The length of dry season is used for reference in calculating water demand. Prediction of drought can be studied based on the rainfall patterns that have occurred. This is possible because there is a tendency that the rain will repeat a certain pattern at a certain time. The purpose of this study was to predict the onset of dry and rainy seasons as well as their length. Determination of the onset of dry season and its length was conducted using polynomial function of the cumulative amount of rain every single day based on the rain data. The research was conducted using rainfall data from Climate Station III in Serang from 1989 to 2010. The sum of daily rainfall could form a polynomial function. If the magnitude of daily rainfall in a certain period of time is less than the slope of the cumulative annual rainfall, then at that time the dry season is occurred. Determination of the dry season peak can be done by finding the maximum (extreme) point from the polynomial function by getting the second derivative which value is close or equal to zero. In average, the dry season occurred in Serang city started on the 132nd until 300th day. Deviation value for the onset of dry and rainy seasons were 23 and 38 days, respectively, with an average of length of 168 days. The average of R2 value for polynomial function was 0.9937.
Co-Authors - Reskiana - Wiranto . Rudiyanto Abiyyu Gustya Putra Adib Khoirul Anas Adlan Adlan Ahmad Abdul Hafiidh Ahmad Fausan Ahmad Fausan Akfia Rizka Kumala Akfia Rizka Kumala, Akfia Rizka Allen Kurniawan Amalia Nurul Huda Amelia, Fatihaturrizky Anas, Adib Khoirul Anastasia Elissa Andiko Putro Suryotomo Anggara, Heru Anna Farida Ardiansyah -- -- Ari Sugiarto Arief Sudarmaji, Arief Arien Heryansyah Armin Zuliarti Bambang Pramudya Bani, Aplonia Nia Blandine Lemercier Blandine Lemercier Bonjok Istiaji Budi I Setiawan Budi Indra Setiawan Chaerur Rozikin Chusnul Arif Daeng Barang, Millah Hudiyah Dedi Kusnadi Kalsim Elissa, Anastasia Endang Gunawan Eni Sumarni Eni Sumarni Erfiana, Eka Erizal Erizal , Erizal -, Erizal Erizal Erizal Euis Kania Kurniawati Fachrudin, Muhammad Fadli Irsyad Febrita, Joana Firdaus, Muhammad Ihsan G. H. Sumartono Gustya Putra, Abiyyu Hafiidh, Ahmad Abdul Hanhan A Sofiyuddin Harry Imantho Helena Ariesty Helena Ariesty Herry Suhardiyanto Heru Sukoco I Dewa Made Subrata IBNUL QAYIM Ihsani, Nanda Nashiha Irsyad Syaifudin Isvan Taufik J. Purwanto, Muhammad Yanuar Joana Febrita Joana Febrita Joko Sumarsono Julianto, Baskoro Tri Kazutoshi Osawa Kazutoshi Osawa Khoirunnisa, Hana Kudang Boro Seminar Lionel Bertheir Lionel Berthier Lisma Safitri Liyantono Luthfi Riady Manik, Ayu Sartika Imia Marhabsyah Zhaki Marzan A. Iskandar Matsuda, Hiroshi Millah Hudiyah Daeng Barang Moh Yanuar J Purwanto Muhamad Askari Muhamad Askari Muhamad Budi Saputra Muhammad Ihsan Firdaus Muhammad Yanuar J. Purwanto Muhammad Yanuar J. Purwanto Muhammad Yanuar J. Purwanto Naufal Rudini Nibras Nasyirah Nora H. Pandjaitan Owen Jacob Notonugroho Pasca Eka Prasetya Popi Redjekiningrum Dwi Mustatiningsih Popi Rejekiningrum Popi Rejekiningrum Prasetya, Dimas Ardi Prastowo Prastowo Prastowo Prastowo Prastowo Purwanto, Moh Yanuar J Purwanto, Mohammad Yanuar J Puspitasari, Putri Arum Putra, Heriansyah Putri Arum Puspitasari Radius Pranoto Rahmat Isnain Ramadhanis, Zainab Dwi Roh Santoso Roh Santoso Budi W Roh Santoso Budi Waspodo Rozikin, Chaerur Rudi Yanto Rudi Yanto, Rudi rudiyanto Rudiyanto . Rusianto Saputra, Muhamad Budi Setiawan , Budi Indra Setjo, Teguh Budiaji Sofiyuddin, Hanhan A. Sudirman Sirait Suprihatin Suprihatin Sutoyo Sutoyo Tamura, Koremasa Teguh Budiaji Setjo Utami, Anisa Dwi Vigie Priantika Putra Hutama Wawan Hermawan Willy Bayuardi Suwarno Wiranto . Yanti Susanti Yanto Surdianto Yanuar Chandra Wirasembada Yanuar Chandra Wirasembada Yanuar Chandra Wirasembada Yayu Romdhonah Yudi Chadirin Zhaki, Marhabsyah Zuliarti, Armin