Judul: Pelapisan Anggota Koperasi Unit Desa (KUD) Gandasari Atas Dasar Pendapatan atau Luas Lahan Garapan dalam Peranannya Terhadap  Keikutsertaan Anggota Studi Kasus di KUD Gandasari, Kec. Plumbon, Kab Cirebon
Abstrak: Tujuan praktek lapang ini adalah untuk mengetahui dan mengikuti kegiatan usaha serta manajemen organisasi KUD, mengetahui pelapisan anggota KUD dan hubungannya dengan besarnya tingkat keikutsertaan anggota, Anggota KUD sebagian besar terdiri dari petani yang tergolong subsisten dan pedagang yang tergolong berpendapatan rendah. Oleh karena kepentingan yang berbeda dari para petani dan pedagang maka tingkat keikutsertaannya juga berbeda.
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Judul: Pengkajian keragaan Koperasi Unit Desa : studi kasus pada KUD Mekar Jaya di Desa Lembursawah, Kecamatan Cibadak, Kabupaten Sukabumi
Abstrak: Tujuan praktek lapangan ini adalah untuk mengetahui keragaan KUD ditinjau dari aspek partisipasi anggota, Organisasi dan manajemen, permodalan dan usaha serta untuk mengetahui klasifikasi KUD berdasarkan penilaian Sarengat. Praktek lapangan dilaksanakan bersamaan waktunya dengan Kuliah Kerja Nyata (KKN), yaitu selama tiga bulan dimulai dari 3 Maret sampai dengan 3 Juni 1986. KUD Mekar Jaya didirikan pada tanggal 25 September Jumlah anggota penuh dan calon anggota sampai akhir 1975. tahun 1985 sebanyak 432 orang. Modal yang telah dikumpulkan dari anggota pada tahun yang sama sebesar 169.3 juta rupiah. Kegiatan usaha KUD terdiri atas bidang usaha eko- nomi yaitu unit penyaluran sarana produksi pertanian dan unit pengadaan pangan. Hasil dari praktek lapangan menunjukkan bahwa tingkat partisipasi anggota relatif rendah, organisasi dan manajemen kurang baik, permodalan masih didominasi modal luar, hanya bidang usaha yang menunjukkan peningkatan. Rendahnya partisipasi anggota erat kaitannya dengan faktor-faktor penyebabnya seperti dasar keanggotaan yang bukan sukarela, dan sikap pengurus yang lebih mementingkan aspek bisnis dibanding aspek sosial...
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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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