cover
Contact Name
-
Contact Email
-
Phone
-
Journal Mail Official
-
Editorial Address
-
Location
Kota bogor,
Jawa barat
INDONESIA
Agromet
ISSN : 01263633     EISSN : 2655660X     DOI : -
Core Subject : Agriculture,
Agromet publishes original research articles or reviews that have not been published elsewhere. The scope of publication includes agricultural meteorology/climatology (the relationships between a wide range of agriculture and meteorology/climatology aspects). Articles related to meteorology/climatology and environment (pollution and atmospheric conditions) may be selectively accepted for publication. This journal is published twice a year by Indonesian Association of Agricultural Meteorology (PERHIMPI) in collaboration with Department of Geophysics and Meteorology, Faculty of Mathematics and Natural Sciences, IPB University.
Arjuna Subject : -
Articles 6 Documents
Search results for , issue "Vol. 28 No. 1 (2014)" : 6 Documents clear
Variabilitas Curah Hujan Indonesia dan Hubungannya dengan ENSO/IOD: Estimasi Menggunakan Data JRA-25/JCDAS Rahmat Hidayat; Kentaro Ando
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 (1010.222 KB) | DOI: 10.29244/j.agromet.28.1.1-8

Abstract

Rainfall variability over Indonesia and its relation to El Niño – Southern Oscillation (ENSO) and the Indian Ocean Dipole (IOD) events were investigated using the Japanese 25-year reanalysis/Japan Meteorological Agency (JMA) Climate Data Assimilation System (JRA-25/ JCDAS). The JRA-25 data consistently depicts seasonal variation of Indonesian rainfall with a wet season that peaks at December-January and a dry season that peaks in July-August when the convection belt moved northward. Composite analysis of rainfall, sea surface temperature and low-level wind anomalies have shown that the impact of ENSO/IOD on rainfall variations in Indonesia is clearly dominant during dry season. Drought conditions typically occur during El Niño years when SST anomalies surrounding Indonesia are cool and walker circulation is weakened, resulting in anomalous surface easterlies across Indonesia. In contrast, in the wet season, the weakening of the relationship between ENSO and Indonesian rainfall is linked to the transition between surface southeasterlies to northwesterlies. At this time persistent surface easterly anomalies across Indonesia superimposed on the climatological mean winds during a warm phase of ENSO event acts to reduce the wind speed resulting reduced the negative DJF rainfall anomalies.
Dynamical Downscaling Luaran Global Climate Model (GCM) Menggunakan Model REGCM3 untuk Proyeksi Curah Hujan di Kabupaten Indramayu Syamsu Dwi Jadmiko; Akhmad Faqih
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 (352.957 KB) | DOI: 10.29244/j.agromet.28.1.9-16

Abstract

Future rainfall projection can be predicted by using Global Climate Model (GCM). In spite of low resolution, we are not able specifically to describe a local or regional information. Therefore, we applied downscaling technique of GCM output using Regional Climate Model (RCM). In this case, Regional Climate Model version 3 (RegCM3) is used to accomplish this purpose. RegCM3 is regional climate model which atmospheric properties are calculated by solving equations of motion and thermodynamics. Thus, RegCM3 is also called as dynamic downscaling model. RegCM3 has reliable capability to evaluate local or regional climate in high spatial resolution up to 10 × 10 km. In this study, dynamically downscaling techniques was applied to produce high spatial resolution (20 × 20 km) from GCM EH5OM output which commonly has rough spatial resolution (1.875o × 1.875o). Simulation show that future rainfall in Indramayu is relatively decreased compared to the baseline condition. Decreased rainfall generally occurs during the dry season (July-June-August/JJA) in a range 10-20%. Study of extreme daily rainfall indicates that there is no significant increase or decrease value.
Prediksi Awal Musim Hujan di Jawa Menggunakan Data Luaran Regional Climate Model Version 3.1 (RegCM3) Fithriya Yulisiasih Rohmawati; Rizaldi Boer; Akhmad Faqih
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 (357.875 KB) | DOI: 10.29244/j.agromet.28.1.17-22

Abstract

Monsoon onset information plays an important role in setting up planting strategy for achieving optimum yield. This study aimed to develop forecasting model for the monsoon onset in main rice growing area of Java used Regional Climate Model Version 3.1 (RegCM3). The forecasting models of the monsoon onset and September-Oktober-November (SON) rainfall data were developed using regression model that have the highest coefficient determination and the models were tested using likelihood ratio test. It was found that the forecasting models of the monsoon onset and September-Oktober-November rainfall data were polynomial orde 2 or cuadratic that have coefficient determination 69%, 74%, 80% and 86%. Likelihood ratio test found that RegCM3 rainfall data was not significantly different with observation rainfall data (α = 0.05). Onset in Java between 25th until 34th of 10-days period (early September until early December).
Kaitan Ruang Terbuka Hijau dengan Kenyamanan Termal Perkotaan Sobri Effendy; Ferdy Aprihatmoko
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 (698.201 KB) | DOI: 10.29244/j.agromet.28.1.23-32

Abstract

The existence of green open space in urban areas is very important in influencing the conditions of thermal comfort. The objective of this research was to analyze the relationship between green open space and human comfort for the city of Yogyakarta. We employed Temperature Humidity Index (THI) with input air temperature and relative humidity. The THI value was obtained from four green open space categories those are point, line, area and non-green space. The results showed that the green open space has a positive effect on lowering the air temperature through the cooling effect and providing more comfortable conditions than the place with non-green open space. Based on this research, the city of Yogyakarta could be categorized as quite comfortable.
Pengaruh Ketinggian Tempat dan Curah Hujan Pada Penyakit Diare (Studi Kasus: Kabupaten Bogor) Muhammad Syafei; Rini Hidayati
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 (347.692 KB) | DOI: 10.29244/j.agromet.28.1.33-39

Abstract

This study aimed to determine the effect of altitude and rainfall on the incidence of disease ( IR ) diarrhea, and to obtain threshold values of rainfall that often cause diarrhea. Determination category of normal rate of diarrhea IR is based on diarrhea IR by DINKES Bogor in the amount of 20-25/1000 population per year, while the determination of precipitation category is based on consideration of Oldeman climate classification. The results showed that there were two districts with very high levels of vulnerability i.e.  Cisarua and Cijeruk, while the other regions only at a moderate level. The negative influence of altitude (or positive influence of temperature) on the IR will be evident if the analysis is separated between in the highlands (> 600 asl) and the lowlands (< 600 asl). This influence is significant, especially at altitudes above 600 meters above sea level. The correlation of the precipitation is significant negative linear to the incidence of diarrhea in the district Cisarua, Cibinong, Jonggol, and Jasinga. In districts Cibinong, Jonggol, and Jasinga, precipitation should be anticipated in the range of 100-200 mm/month, where moderate IR often occurs, while in the district Cisarua, is in the range of precipitation 300-400 mm/month, where high IR often occurs.
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.

Page 1 of 1 | Total Record : 6


Filter by Year

2014 2014


Filter By Issues
All Issue Vol. 39 No. 2 (2025): DECEMBER 2025 Vol. 39 No. 1 (2025): JUNE 2025 Vol. 38 No. 2 (2024): DECEMBER 2024 Vol. 38 No. 1 (2024): JUNE 2024 Vol. 37 No. 2 (2023): DECEMBER 2023 Vol. 37 No. 1 (2023): JUNE 2023 Vol. 36 No. 2 (2022): DECEMBER 2022 Vol. 36 No. 1 (2022): JUNE 2022 Vol. 35 No. 2 (2021): DECEMBER 2021 Vol. 35 No. 1 (2021): JUNE 2021 Vol. 34 No. 2 (2020): DECEMBER 2020 Vol. 34 No. 1 (2020): JUNE 2020 Vol. 33 No. 2 (2019): DECEMBER 2019 Vol. 33 No. 1 (2019): JUNE 2019 Vol. 32 No. 2 (2018): DECEMBER 2018 Vol. 32 No. 1 (2018): JUNE 2018 Vol. 31 No. 2 (2017): DECEMBER 2017 Vol. 31 No. 1 (2017): JUNE 2017 Vol. 28 No. 1 (2014) Vol. 25 No. 1 (2011): JUNE 2011 Vol. 24 No. 2 (2010): DECEMBER 2010 Vol. 24 No. 1 (2010): JUNE 2010 Vol. 23 No. 2 (2009): December 2009 Vol. 23 No. 1 (2009): June 2009 Vol. 22 No. 2 (2008): December 2008 Vol. 22 No. 1 (2008): June 2008 Vol. 21 No. 2 (2007): December 2007 Vol. 21 No. 1 (2007): June 2007 Vol. 20 No. 2 (2006): December 2006 Vol. 20 No. 1 (2006): June 2006 Vol. 19 No. 2 (2005): December 2005 Vol. 19 No. 1 (2005): June 2005 Vol. 18 No. 2 (2004): December 2004 Vol. 18 No. 1 (2004): June 2004 Vol. 17 No. 1 & 2 (2003): June 2003 Vol. 16 No. 1 & 2 (2002): December 2002 Vol. 15 No. 1 & 2 (2000): DECEMBER 2000 Vol. 14 No. 1 & 2 (1999): June 1999 Vol. 13 No. 2 (1998): december 1998 Vol. 13 No. 1 (1998): JUNE 1998 Vol. 12 No. 1 & 2 (1997): DECEMBER 1996/1997 Vol. 11 No. 1 & 2 (1995): DECEMBER 1995 Vol. 10 No. 1 & 2 (1994): DECEMBER 1994 Vol. 9 No. 2 (1993): December 1993 Vol. 9 No. 1 (1993): June 1993 Vol. 8 No. 1 (1992): June 1992 Vol. 7 No. 2 (1991): DECEMBER 1991 Vol. 7 No. 1 (1991): JUNE 1991 Vol. 6 No. 1 (1990): JUNE 1990 Vol. 5 No. 1 (1989): June 1989 More Issue