Judul: Preferensi Dan Pola Konsumsi Suplemen Makanan Yang Mengandung Serat
Abstrak: Tujuan Umum dari penelitian ini adalah untuk mengetahui preferensi dan pola konsumsi suplemen makanan yang mengandung serat. Sedangkan tujuan khusus dari penelitian ini adalah untuk mengetahui karaktenstik individu dari konsumen yang mengkonsumsi dan tidak mengkonsumsi suplemen makanan yang mengandung serat, mengetahui pola konsumsi konsumen suplemen makanan yang mengandung serat, mempelajari faktor-faktor yang berhubungan dengan pola konsumsi suplemen makanan yang mengandung serat, mengetahui preferensi konsumen terhadap suplemen makanan yang mengandung serat.
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Judul: Studi tentang Pola Konsumsi Serat Pada Mahasiswa
Abstrak: Penelitian ini didesain dengan metode penelitian survai (cross-sectional) yang dilakukan di Bogor, Kampus Institut Pertanian Bogor (IPB). Penelitian ini dilakukan mulai bulan Januari sampai bulan Mei 2004. Contoh dalam penelitian ini adalah mahasiswa. Golongan mahasiswa dipilih sebagai contoh karen a mereka termasuk individu yang berisiko mengalami kurang serat yang dapat berdampak pada munculnya gangguan penyakit degeneratif di kemudian hari. Contoh mahasiswa yang dipilih sebanyak 60 orang mahasiswa terdiri ~dari 30 orang mahasiswa GMSK dan 30 orang mahasiswa Kehutanan. Contoh dipilih secara purposive sampling dengan pertimbangan contoh bemsia 18-22 tahun, angkatan 38 atau telah mejalani kuliah minimal selama 6 semester .. J enis data yang dikumpulkan adalah data primer meliputi : data identitas respond en, pengetahuan dan sikap gizi, faktor sosial/ekonomi, ketersediaan, pola konsl!msi, tingkat konsumsi makanan yang mengandung serat, dan aspek kesehatan. Data dikumpulkan dengan cara wawancara menggunakan kuesioner. Data konsumsi makanan diambil dengan carafood recall 1 X 24 jam, kemudian dikonversi dengan menggunakan Daftar Komposisi Bahan Makanan Malaysia (1997). Data kebiasaan dan frekuensi makan dikumpulkan dengan cara wawancara mengggunakan metode food frequency questionnare (Sanjur &Rodriquez, 1997).
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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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