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: Pertumbuhan dan tingkat kelangsungan hidup larva ikan betutu, Oxyeleotris marmorata (Blkr.), yang diberi pakan alami infusoria
Abstrak: Penelitian ini bertujuan untuk mengetahui pertumbuhan tingkat kelangsungan hidup larva ikan betutu, dan Oxyeleotris marmorata (Blkr.), yang diberi pakan alami infusoria, dan dilaksanakan pada tanggal 19 Februari sampai 3 Maret 1991 di Kolam Babakan Darmaga, Bogor. Infusoria diberikan ke larva ikan betutu dengan kepadatan 100, 500 dan 900 individu/ml, masing-masing dengan tiga kali ulangan. Larva ikan dipelihara dalam akuarium dengan volume air sebanyak 40 liter dan kepadatan larva 40 ekor/liter. Penggantian air dilakukan setiap hari sebanyak 20% dari volume air sebelum pemberian pakan (pagi hari). Pengambilan contoh ikan sebanyak 10 ekor dilakukan 3 hari sekali. Dalam perut larva tidak ditemukan adanya infusoria sehingga diduga infusoria tidak dimakan oleh larva. Infusoria yang tumbuh dalam media kultur adalah dari jenis Euglena sp., Chilodonella sp. dan Vorticella sp.. Bobot larva ikan betutu menurun selama pemeliharaan. Laju pertumbuhan dan kelangsungan hidupnya meningkat masing-masing dari 7,55 hingga 3,11% per hari dan dari 1,94 hingga 3,40% dengan meningkatnya pemberian infusoria dari 100 hingga 900 individu/ml.
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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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