Judul: Perbanyakan Bibit Tanaman Hortikultura dan Permasalahannya di Kebun Pembibitan Ragunan dan Ciganjur Dinas Pertanian DKI Jakarta
Abstrak: Tujuan pengembangan produksi hortikultura terutama dimaksudkan untuk (1) memperbaiki gizi masyarakat, terutama yang berpenghasilan rendah, (2) memperbesar devisa negara dengan mengurangi impor dan meningkatkan ekspor, (3) memperluas kesempatan kerja dan meningkatkan pendapatan masyarakat, dan ( I + ) memenuhi kebutuhan akan keindahan dan kesesuaian lingkungan.
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Judul: Pelaksana praktek lapang di kebun hortikultur cibubur dan lebak bulus dinas pertanian DKI Jakarta
Abstrak: Indonesia adalah negara agraris yang mempunyai potensi lahan pertanian yang sangat luas dan jenis tanaman tropikanya yang amat beragam. Potensi yang demikian ini belum mampu dimanfaatkan secara optimal. Hingga saat ini Indonesia masih mengimpor produk pertanian dalam jumlah besar bukan saja berupa bahan makanan pokok yaitu beras, tetapi juga yang digolongkan dalam komoditi hortikultura. Pada th 1982 Indonesia mengimpor komoditi hortikultur sebesar 49.912,16 ton berupa jeruk, apel, anggur, dan bawang (Bank Bumi Daya, 1984). Walaupun Indonesia mengimpor komoditi hortikultur bukan berarti sama sekali tidak mampu untuk menghasilkan produk hortikultur dalam jumlah yang cukup atau bahkan surplus untuk kebutuhan dalam negri. Pada th 1982 Indonesia mampu mengekspor komoditi hortikultur sebesar 36.516,5 ton berupa mangga, adpokat, kentang, kubis, bawang merah, dam sayuran segar lainnya (Bank Bumi Daya, 1984). Komoditi hortikultur amat banyak jenisnya, maka impor yang dilakukan Indonesia bisa disebabkan oleh kurang intensifnya produksi suatu jenis komoditi, rendahnya kwalitas, atau bertambahnya permintaan terhadap suatu komoditi. Seperti misalnya pada anggur, peningkatan impor anggur segar dari th 1978 sebesar 1.927,88 ton hingga th 1982 menjadi sebesar 2.817,16 ton karena adanya peningkatan permintaan anggur dalam negri (Bank Bumi Daya, 1984).
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Judul: Thermal Characteristics and Dynamics of Tropical Cyclone over Western North Pacific Ocean: A Case Study of Typhoon Songda (Chedeng) 2011
Abstrak: The frequent occasion of Tropical Cyclone (TC) over Western North Pacific (WNP) Ocean lies from 10˚N to 26˚N and 121˚E to 170˚E. Sources of TC development come from warm ocean temperature where latent heat is released during condensation processes and subsequently concentrated in the boundary layer. Relative humidity at 850-700 hPa is responsible to produce the most intense storm. Meanwhile, weak vertical wind shear between 850-200 hPa is one of the dynamical factors that lead to the development of TC. Pressure level of 850-200 hPa is chosen to minimize the thermodynamic effect in the lower troposphere. Typhoon Songda (Chedeng in the Philippines) or TSC lasted from May 18th to 30th, 2011 and strengthened into powerful Super Typhoon stage between May 24th and 27th. Long curving track and the exhibition of all sequences of TC life cycle, TSC is then considered as an ideal case of TC. The objective of the study with case of TSC is to investigate the role of thermal characteristics and dynamics on TC intensity. The research is carried out by using Advanced Research of Weather Research and Forecasting model (WRF ARW model) version 3.3. Two domains are employed in the model. The first domain situate from 02˚N to 40˚N and 118˚E to 149˚E and cover spatial resolution () of 33.1 km. The second domain situate from 09˚N to 27˚N and 119˚E to 132˚E with of 11 km. Timestep of the model () is 120 seconds. The model is supported by the following physical parameterization, i.e., Yonsei University Scheme (YSU) in the boundary layer, Kain-Fritsch scheme (KF) in the cumulus, and WRF Single-Moment 3-class scheme in the microphysics. Initial meteorological condition prior to the formation of the cyclone is generated using WRF ARW standard-release model. Sensitivity of the model output is obtained from a selected single-parameter change scenarios, namely, 10 % to 20 % decrease and increase of wind shear initial data at 850-200 hPa, and by 10 % to 20 % decrease of relative humidity initial data at 850-700 hPa. The result showed that the negative correlations between wind shear and intensity are found in wind shear scenarios. Wind shears of 10 ms-1 which lead to strengthening of the wind intensity in the early period of Typhoon development are found in wind shear scenarios. The effect of wind shear changes on wind intensity is statistically significant in the 20 % wind shear scenarios. During mature stage, weak wind intensity occurred when wind shear increase as given in the WRF standard-release and the 20 % decreasing scenario. Different situation is found in the 20 % increasing scenario where wind shear tend to weak and lead to strong wind intensity at this stage. Meanwhile, the reduction of moisture supply at 850-700 hPa resulting from 20 % decreasing relative humidity play a major role in the weakening of wind intensity and reduces mechanical energy of the cycle process as much as 300 J kg-1.
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