Judul: Rendezvous Search Pada Garis Dengan Lebih Dari Dua Pemain
Abstrak: Pada suatu jalan raya, lebih dari dua orang yang bersahabat, telab sepakat akan bertemu di jalan tersebut, tetapi mereka tidak tahu di mana letak sebenarnya mereka akan bertemu. Pencarian dilakukan sepanjang jalan raya tersebut dan untuk memecahkan masalah ini digunakan rendezvous search pada garis. Penelitian ini dilakukan untuk membanlu para pemain agar mereka dapal bertemu datam waktu yang minimum. Pada awal penempatan di jalan raya, setiap pemain mengetahui posisi masing-masing tetapi tidak mengetahui posisi pemain lain. Mereka bergerak dengan kecepatan paling besar 1 untuk bertemu.
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Judul: Rendezvous Search Pada Garis Dengan Tiga Pemain
Abstrak: Pada suatu lapangan luas dengan lintasan kereta api melintasi seluruh daerah tersebut, tiga orang penerjun ditetjunkan. Mereka telah menyepakati sebelumnya untuk bertemu di I[ntasan kereta api tersebut, tetapi belum tahu letak yang sebenarnya untuk bertemu. PenCanan dilaknkan di sepanjang lintasan kereta api dan untuk memecahkan masalah ini digunakan rendezvous search pada garis.
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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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