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Agromet

agromet
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Published by Institut Pertanian Bogor

ISSN : 01263633 EISSN : 2655660X DOI : -

Core Subject : Agriculture,

Agriculture, Biological Sciences & Forestry

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 5 Documents

Search results for , issue "Vol. 20 No. 2 (2006): December 2006" : 5 Documents clear

EVALUASI DAMPAK PERUBAHAN PENGGUNAAN LAHAN TERHADAP VOLUME LIMPASAN STUDI KASUS: DAS CILIWUNG HULU, JAWA BARAT (EVALUATION OF LANDUSE CHANGE IMPACT ON RUN-OFF VOLUME CASE STUDY : CILIWUNG HULU WATERSHED, WEST JAVA) B. D. Dasanto; . Risyanto
Agromet Vol. 20 No. 2 (2006): December 2006
Publisher : PERHIMPI (Indonesian Association of Agricultural Meteorology)

The upper Ciliwung watershed is one of the critical catchments areas in Java Island. A major element of this area is the modification of natural land-cover due to human activities. Land use change is driven by the interaction between physical and socio-economic factors. The objective of this paper is to develop a land use change model and to evaluate runoff volume based on land use prediction. The pseudo-R2 or 2 in this model is 51.7% and the calibration between predicted land use and the real is 65.5%. The analysis result of land use change for period 2005-2010 and 2015-2020 show a special change pattern. In the first period, the forest land will decrease by 85%, while resettlements land increase by 144%, so the Curve Number value will increase from 80 to 81. These indicate decreasing capability of the upper Ciliwung to retain rainfall. The impact of this condition will increase runoff volume from 660.000 m3 to be 905.000 m3. In the second period, the forest and resettlements land will increase by 612% and 28%, so the Curve Number will decrease from 80 to be 78. This will decrease runoff volume from 805.000 m3 to be 803.000 m3.

PEWILAYAHAN AGROKLIMAT TANAMAN NILAM (Pogostemon spp.) BERBASIS CURAH HUJAN DI PROVINSI LAMPUNG (AGROCLIMATE ZONING OF PATCHOULY (Pogostemon ssp.) BASED ON RAINFALL IN LAMPUNG PROVINCE) I. G. Darmaputra; Y. Koesmaryono; I. Santoso
Agromet Vol. 20 No. 2 (2006): December 2006
Publisher : PERHIMPI (Indonesian Association of Agricultural Meteorology)

The research purposed to determine the patchouly cropping in Lampung Province based on the agroclimate feasibility of area rainfall and to determine the monthly rainfall probability which less than the patchouly requirement. There are four steps on this research such as to determine the seasonal rainfall distribution by Principle Component Analysis, seasonal rainfall zoning by Cluster Analysis, and agroclimate zoning of patchouly by superimpossed annual region rainfall map, regional map of wet month, topography map to patchouly agroclimate requirement, and to determine the monthly rainfall probability which less than the patchouly crop requirement. The result of research shows 2,069,005 ha of Lampung Province area most feasible and feasible to patchouly cropping, which are spread in Lampung Barat Regency (15.7%), Lampung Tengah Regency (15.5%), Way Kanan Regency (14.3%), Tanggamus Regency (14%), Lampung Utara Regency (12.5%), Lampung Timur Regency (10.8%), Tulang Bawang Regency (8.5%), Lampung Selatan Regency (8.2%), Bandar Lampung City (0.4%) and Metro City (0.1%). The results also reveal that the seasonal rainfall in Lampung Province can be grouped in seven types (I-VII), and the most feasible area lay on type I-IV, but for feasible area lay on type I-VI. Related to rainfall probability, at type I there is not occured monthly rainfall ≤ 200 mm with probability ≥ 60%, where as at type II the condition can be occurred 5 months, at type III and IV occurred 4 months, and at type V and VI occurred 7 months.

ANALISIS POLA UNSUR METEOROLOGI DAN KONSENTRASI POLUTAN DI UDARA AMBIEN STUDI KASUS : JAKARTA DAN BANDUNG (ANALYSIS OF PATTERN OF METEOROLOGY VARIABLE AND AMBIENT POLUTANT CONCENTRATION CASE STUDY : BANDUNG AND JAKARTA) A. Turyanti; I. P. Santikayasa
Agromet Vol. 20 No. 2 (2006): December 2006
Publisher : PERHIMPI (Indonesian Association of Agricultural Meteorology)

Meteorological conditions are the important factors that influence tranformation and tranportation process of the polutant in the atmosphere. The aim of this research is to study correlation between local meteorology condition with ambient polutant concentration. Case study has been done in Jakarta and Bandung. Research method is secondary data analysis by plot meteorology component (radiation, temperature, hummidity and wind velocity) and polutant consentration, to gain fluctuation pattern from both component and than do correlation analysis. Result of the analysis show that the influence of each meteorology component differ to each polutant component and depend on local condition. In Bandung and Jakarta, radiation fluctuation has negative correlation with CO, NO2, Nox and PM10. The most negative correlation in Bandung is wind velocity with CO which has correlation value -0.74, and correlation between humidity and O3 which has value -0.8. While the most positive correlation is correlation between temperature and radiation with O3 which has value 0.7 – 0.8. Humidity has positive correlation with several polutant. In Jakarta, in general, coefisien correlation value both positive and negative correlation less than coefisien correlation in Bandung, except for O3. The influence of amount and kind of emition also contribute to them. The unique matter has been found that meteorology component fluctuation in both Jakarta and Bandung has high correlation positive and negative with O3, up to the value -0.8 to +0.7. The other polutant component has small in both negative and positive cerrelation (±0.5).

DAMPAK VARIABILITAS IKLIM MUSIMAN PADA PRODUKSI PADI SAWAH TADAH HUJAN DI PULAU LOMBOK (IMPACT OF INTERANNUAL CLIMATE VARIABILITY ON RAINFED PADDY PRODUCTION IN LOMBOK ISLAND) I. Yasin; M. Ma'shum
Agromet Vol. 20 No. 2 (2006): December 2006
Publisher : PERHIMPI (Indonesian Association of Agricultural Meteorology)

Variability of inter-anuual rainfall has great impact on agricultural production. The inter-annual rainfall variability mainly causes cropping and harvest failure in rainfed land due to drought and flood. Although the onset of season is usully known, the characteristic of in coming rainfall is usually not predictable. Thus the understanding of the cause of rainfall variability may lead to establishment of new system to forecast seasonal rainfall characteristics. The aims of this research are to study water availibity for dry direct seeding rice by considering water balance in southern Lombok and understanding the relationship between ENSO phenomena with rain event in Lombok as well using SOI for predicting seasonal rainfall events. The results of this research showed that average rainfall in southern Lombok is 1450 mm with 950 mm the lowest and 2460 the highest. Southern Lombok has three water surplus months (with rainfall >200 mm), and 5 to 6 water deficit months (with less than 100 mm rainfall).. Inter annual rainfall variation is closely correlated to ENSO phenomena where the rainfall tend to be obove normal in La Niña years and below normal in El Niño years. The short term wet months and wide range of rainfall varibility lead to the need to establishment of water storage system and the application of water and cropping management which suitable to rainfall characteristics and local environmental conditions. The use of ENSO and SOI value to forecast seasonal rain events may be suitable and may reduce the risks of cropping system in rainfed agricultural land.

ANALISIS PELUANG DERET HARI KERING PADA TANAMAN PADI TADAH HUJAN DI KABUPATEN KULONPROGO DALAM PERSPEKTIF TOPOSEKUENS (PROBABILITY ANALYSIS OF DRY SPELL ON RAINFED PADDY AT KULON PROGO DISTRICT IN TOPOSEQUENCE PERSPECTIVE) F. Fibrianty; S. Sarjiman
Agromet Vol. 20 No. 2 (2006): December 2006
Publisher : PERHIMPI (Indonesian Association of Agricultural Meteorology)

Climate anomaly has significant impact on rainfall and its pattern, whereas they were important factor in determining onset of wet and dry season. Changes in rainfall pattern need to antisipate with tailoring planting date for minimize harvest risk. This research purpose to analyse dry spell probability and its relation to drought risk on rainfed paddy at Kulon Progo District in Toposequence Perspective.Kulon Progo District was divided into three sequence, that were Fluvial as catchment area (i.e. Samigaluh); Freatik as conservation area (i.e. Kenteng, Kalibawang and Kokap); and Fluksial as user area (i.e. Gembongan- Sentolo, Sapon-Lendah and Wates). The aimed of this research was to analyze the drought periods and its relation with drought risks on rainfed rice plant at Kulon Progo district in toposequence perspective. The probabilities of 15 day dry spell at Fluvial area were 0,27 – 0,44 on May-September. On Freatik area, the probabilities of 15 day dry spell were 0,21 - 0,43 on April-Oktober at Kenteng, while at Kalibawang and Kokap the probabilities were > 0,2 on May-September. The probabilities at Gembongan-Sapon were> 0,2 on May-October, while at Wates the probabilities on May-September were 0,21-0,32. The distribution of probability show that the probability of 15 day dry spell were > 0,2 at May-October and the driest periods were August-September but with various dry level, that Kenteng and Gembongan-Sapon were the driest area. Based on that analysis, the planting periods should be started on November and the last planting should not over than January, especially at Kenteng, Gembongan and Sapon.

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