Judul: Sistem Informasi Kenaikan Pangkat Kepegawaian
Abstrak: Untuk dapat dinaikan pangkalnya. seorang Pegawai Negeri Sipil harns memenuhi syarat-syarat Ketentu. Untuk mempercepat proses pengusulan kenaikan pangkat dan penelusuran informasi. dibutuhkan suatu sistem yang secara ako111odatif mendukung manajemen kepegawaian untuk mendapatkan informasi yang diperlukan. Sistem lnformasi Kenaikan Pangkal Kepcgawaian (SIKPK) adalah suatu sistem informasi yang dapal Imempercepat proses pcngusulan kenaikan pangkal dan memberikan sejumlah informasi yang diperlukan. sehingga membantu manajemen kcpcgawaian dalam memproses pengusulan kenaikan pangkat pegawai.
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Judul: Perancangan Antarmuka Pengguna Sistem Informasi Kenaikan Pangkat di BPPT Menggunakan Metode Galitz
Abstrak: Badan Pengkajian dan Penerapan Teknologi (BPPT) mulai menerapkan pelayanan teknologi informasi untuk membantu dalam penyebaran informasi kepada seluruh pegawai yang tersebar di beberapa kota seperti Jakarta, Serpong, Lampung, Yogyakarta, Surabaya, dan Denpasar. Maka Biro Sumber Daya Manusia dan Organisasi ingin meningkatkan pelayanan kepegawaian dalam proses kenaikan pangkat pegawai. Selama ini proses pengumpulan persyaratan kenaikan pangkat (KP) masih dilakukan dengan mengumpulkan berkas-berkas langsung ke sekretariat sehingga prosesnya memakan waktu lebih lama. Maka dari itu agar proses pengumpulan persyaratan KP berjalan lebih baik diperlukan suatu aplikasi yang dapat membantu dalam proses manajemen KP, dimulai dari membuat usulan KP, persetujuan atasan dan mengunggah dokumen persyaratan. Untuk mempermudah proses KP ini dirancang antarmuka pengguna Sistem Informasi Kenaikan Pangkat dengan menggunakan Metode Galitz.
Keyword: kenaikan pangkat, metode galitz, pelayanan kepegawaian

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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