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"Banyaknya benda berosilasi yang gerak bolak baliknya tidak dapat sama karena gaya gesekan melepaskan tenaga geraknya. Untuk menentukan nilai momen inersia pada benda pejal yang beraturan dapat dengan mudah dihitung akan tetapi untuk menghitung nilai momen inersia pada benda pejal yang tidak beraturan sangatlah susah sehingga penelitian ini dilakukan. Pengukuran ini menghubungkan persamaan osilasi dengan persamaan momen inersia yang dialami benda pejal. Besarnya redaman dihitung dari data osilasi percepatan yang diperoleh melalui rangkaian mikrokontroler dengan accelerometer sebagai sensornya. Data osilasi percepatan kemudian ditampilkan melalui komputer dengan pemrograman LabView sebagai Graphical User Interface nya.The oscillating motion of many objects beyond cannot be the same pace because of the friction force releases its motion. To determine the value of moment inertia of a rigid body can be calculated but irregular to calculate the value of moment of inertia in rigid body are very difficult irregular so that the research was done.Measurement of oscillation equation connects the Newton?s law equation with moment of inertia disc-shaped objects going round and square-shaped disc. Relation from these equation shows that the damping coefficient will influence by viscosity coefficient from fluid that measured. The damping coefficient calculates from acceleration oscillation data which get from microcontroller circuit with accelerometer as a sensor. The acceleration oscillation data then displayed on computer with LabView programming as the Graphical User Interface."

"ABSTRACTThe presented study is focused on experimental investigation of a boundary layeron a flat plate in an adverse pressure gradient. The flat plate is placed in a regular flow, thepressure gradient is generated by the plate inclination. The preceding studies deal with thestructure of the wake behind the plate, the presented study concentrates on the flow structureclose to the suction surface of the plate. The dynamical behavior of the flow structures is studiedin details with respect to the topology in the streamwise direction. In spite of the fact that thetime-mean flow field is close to 2D, more or less constant along the span, the instantaneousstructures topology is fully 3D. Rather oblique structures are detected instead of those orientedin the streamwise direction. The patterns are travelling in the streamwise direction along theplate."

"Madden Juliaan Oscillation MJO merupakan fluktuasi intraseasonal berupaosilasi tekanan yang terjadi di wilayah equator. Tujuan penelitian ini adalahmengkaji proses perambatan MJO serta hubungannya dengan arus permukaanlaut, suhu permukaan laut SPL dan curah hujan. Rata-rata kecepatan penjalaranMJO berdasarkan analisis diagram Hovmoller adalah 5 m/s. Berdasarkan hasilanalisis komposit arus menunjukan adanya anomali negatif yang signifikan diLaut Flores pada periode DJF Desember-Februari-Maret dengan anomalisebesar -150 cm/s. Respon suhu permukaan laut menunjukan nilai korelasi kuatantara SPL dan OLR saat fase aktif MJO, dimana MJO terjadi lebih dulukemudian diikuti respon penurunan SPL di wilayah equator. Efek MJO terhadappenambahan curah hujan di wilayah Indonesia bagian Barat sebelah Utara kurangberperan, sementara untuk wilayah tengah Indonesia cukup bervariasi, kondisi inidisebabkan MJO telah berinteraksi dengan fenomena diurnal di Benua MaritimIndonesia.

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Madden Juliaan Oscillation MJO is an intraseasonal fluctuation that oscillatesthe pressure occurring in the equatorial region. The purpose of this research is tostudy MJO propagation process and with sea climate, sea surface temperature SST and rainfall. The average MJO propagation speed based on the Hovmollerdiagram diagram is 5 m s. Based on the results of composite analysis the currentshows a significant negative anomaly in the Flores Sea in the DJF December January February, period with an anomaly of 150 cm s. The sea surfacetemperature response shows a strong correlation value between SPL and OLRduring the active phase of MJO, where MJO occurs first then followed by thedecreasing response of SPL in the equator region. The effect of MJO on theaddition of rainfall in the western part of Indonesia, especially the northern parthas less role, while for the middle region of Indonesia is quite varied, thiscondition is caused by MJO has interact with diurnal phenomenon in IndonesianMaritime Continent."

"Dalam skripsi ini akan dibahas mengenai tingkah laku ayunan tanpa redaman dan dengan redaman yang dihasilkan berdasarkan bentuk penyelesaian persamaan differensial ayunan nonlinier pada bidang fase."

"This monograph explores nonoscillation and existence of positive solutions for functional differential equations and describes their applications to maximum principles, boundary value problems and stability of these equations. In view of this objective the volume considers a wide class of equations including, scalar equations and systems of different types, equations with variable types of delays and equations with variable deviations of the argument. Each chapter includes an introduction and preliminaries, thus making it complete. Appendices at the end of the book cover reference material."