Judul: Sistem Pengadaan Bahan Baku Kayu Bulat Jati Pada lndustri Pengolahan Kayu Jati Swasta di Semarang
Abstrak: Perum Perhutani merupakan salah satu Badan Usaha Milik Negara sebagai pengelola hutan nasional di bawah pembinaan Departemen Kehutanan dan Perkebunan, di dalamnya terdapat upaya agroindustri berupa industri perkayuan, mengupayakan perolehan nilai tambah yang besar dari komoditi tersebut. Produk utama pengusahaan hutan produksi di Perum Perhutani adalah berupa kayu bulat jati. Sejak diterapkannya larangan ekspor kayu bulat, semua kayu bulat jati yang dihasilkan oleh Perum Perhutani diperdagangkan di dalam negeri. Pemasaran di dalam negeri sampai saat ini dilaksanakan melalui cara lelang I dan non lelang. Kegiatan peningkatan nilai tambah bahan baku menjadi produk tertentu, akan melibatkan faktor produksi tertentu (bahan baku, tenaga kerja, modal dan keahlian). Berhubungan dengan kebutuhan bahan baku yang semakin meningkat sejalan dengan meningkatnya industri pengolahan kayu jati, maka dapat menyebabkan persediaan bahan baku kayu bulat jati semakin terbatas, apalagi dengan semakin menurunnya produksi kayu bulat jati oleh Perum Perhutani dan semakin meningkatnya harga kayu bulatjati.
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Judul: Studi Produksi, Pemanfaatan dan Pemasaran Sortimen Pendek kayu Bundar Jati Non Penghara Industri Finir di KPH Cepu
Abstrak: Sumber daya hutan memiliki nilai ekonomis apabila telah dikeluarkan dari hutan. Kayu jati (Tectonn grandis Li~m. F.) sebagai salah satu suinber daya yang merupakan tanaman andalan PT Perhutani men~iliki harga jual yailg mahal dan prospek pernasaralumya cukup cerah. Kayu jati mempunyai nilai yang kl~usus dan arti tradisional bagi orang Indonesia, sehingga dapat memberikan tingkat status sosial terutama kepada peinilik barang yang terbuat dari kayu jati. Hal tersebut tnendorong tunbbuhlya industri-industri besar seperti industri veneer, plyuood, pengusaha lneubel Qiurniture), dan industri kecil laimlya yang membutuhkan bahan baku sehingga perinintaan akan kayu jati jadi meningkat.
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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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