Judul: Perkembangan larva ikan betutu Oxyeleotris marmorata (BLKR), yang dipelihara di kolam dan di tangki
Abstrak: Penelitian perkembangan ini bertujuan untuk mengetahui perbedaan perkembangan larva ikan betutu yang dipelihara di kolam dan tangki. Pemeliharaan larva dilakukan didalam hapa berukuran 1x1x0,8 m berukuran yang dibenamkan di kolam beton berukuran 4x2x0,6m yang telah ditumbuhi pakan alami. Penumbuhan pakan alami dengan cara pengeringan selama 2 hari, lalu dipupuk dengan 100g kotoran ayam/2 dan diairi setinggi 20cm. Tiga hari kemudian dilakukan penyemprotan diazinon 60 EC dengan dosis 7mg/1. Jumlah larva yang dipelihara dihapa adalah 14 ekor/1. ..dst
Keyword: Oxyeleotris marmorata, Ikan betutu, Larva ikan, Pakan ikan

Judul: Perkembangan larva ikan betutu, Oxyleotris marmorata (Blkr.)
Abstrak: Percobaan ini bertujuan untuk mengetahui perkembangan larva ikan betutu mulai dari saat menetas sampai mencapai bentuk definitif (bentuk menyerupai induknya). Percobaan dilakukan di Laboratorium Fakultas Perikanan, Institut Pertanian Bogor, Darmaga dari tanggal 8 Juli sampai 4 Agustus 1990. Bahan yang digunakan adalah telur ikan betutu: hasil pemijahan secara semi alami di kolam. Penetasan dilakukan di akuarium sedang pemeliharaan larva di kolam yang dipupuk. Larva yang digunakan adalah yang menetas pada hari ketiga. Pemberian plankton yang lolos saringan 100 dilakukan pada larva umur satu hari sampai 1,5 hari, yaitu: saat larva menjelang ditebar ke kolam pendederan. Penga- matan larva dilakukan secara mikroskopis dan aspek yang diamati meliputi: diameter kuning telur, diameter butir minyak, diameter mata, panjang total, panjang dari mulut ke anus, tinggi bukaan mulut maksimum, tinggi badan, perkembangan sirip, sisik, pigmen, bobot larva, jenis dan jumlah jasad pakan yang terdapat dalam saluran pencernaan: serta persentase larva yang makan.
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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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