Judul: Variability of chlorophyll-a and some oceanographic parameter in related with monsoon, ENSO and IOD at the Banda Sea.
Abstrak: The Banda Sea is a very fertile area because it’s a potential area of fisheriesfield, and is one of the largest fishing areas in Indonesia. The Banda Sea is influenced by external factors such as El Nino Southern Oscilation (ENSO), the cross-currents of Indonesia (Arlindo) and season. Furthermore the Banda Sea can also be called “the heart of “ current flow in the waters of Indonesia, as well as “the capasitor of ”water mass transport to the Indian Ocean and one of the areas that upwelling occurs where the water surface temperature can reach down to 25oC, was caused by the cold water from the bottom layer is elevated to the upper layers. The purpose of this study was to analyze the influence of variability of sea surface height parameter, sea surface temperature and chlorophyll-a; to analyze the influence of ENSO and Indian Ocean Dipole (IOD) has related with the variability of sea surface height (SSH), sea surface temperature (SST) and chlorophyll-a; and to search the internal forcing that causes the variability. The research was carried out in February 2011-June 2012, located in the Banda Sea with position between 3.5-7.5oLS and 124-133oBT. The data used are the sea surface height, sea surface temperature, chlorophyll-a, which are derived from MODIS-Aquamulti-sensor satellite data from 2002 to 2012, and surface wind data obtained from the European Centre for Medium-Range Weather Forecasts (ECMWF). The data were analyzed by using the Ferret software version 6.0 in order to show the view variability of seasonal cycle and it’s annual cycle. Then the wind data, the Nino index 3.4 and Dipole Mode Index (DMI) will be analyzed by using wavelet methods in Matlab 2010 software to show annual cycle in the format of continous wavelet transform (CWT) and cross wavelet transform (XWT). In the variabilityof monthly average sea surface height from 2002 to 2012, there were the maximum value in March (transitional season I) with the value is 0.1498 m. The sea surface height of minimum in August with the value is -0.02 m. The Variability of sea surface temperature is maximum in December (west season) with a value is 30.68oC. The lowest temperature value found in August with avalue was 26.67oC. The value of chlorophyll concentrationat west ranged from 0.125-0.145 mg/m3 and chlorophyll concentration value at transitional season II ranged from 0.125 to 0.146 mg/m3. The chlorophyll concentration values at east season are 0.285 to 0.458 mg/m3 and chlorophyll concentration value at transitional season I range between 0.372-0.134 mg/m3. The highest value of the chlorophyll concentration which occurs on east season in August with a value of 0.458 mg/m3 and the lowest at west season in December with a value of 0.125 mg/m3. Zonal wind circulation patterns in January (west season) with speed 5.32 m/sec is more stronger because occurrence of the southwest monsoon winds are blown strong whereas in July (east season) the wind speed are weaker at -4,987 m/sec. The meridional wind circulation patterns in July (east season) are more powerful with a value 5.252 m/sec, where happened is south eastern wind monsoon while in February
Keyword: Annual and interannual cycles, multi-sensors satellite data, ENSO, IOD

Judul: Variabilitas Suhu Permukaan Laut dan Konsentrasi Klorofil-a di Samudera Hindia Bagian Timur Laut Sebelah Barat Sumatera
Abstrak: Suhu Permukaan Laut (SPL) dan konsentrasi klorofil-a merupakan parameter penting di dalam suatu perairan dan memiliki kaitan erat terhadap terjadinya fenomena oseanografi dan tingkat produktifitas. Tujuan penelitian ini adalah menganalisis variabilitas SPL dan konsentrasi klorofil-a di Sekitar Samudera Hindia bagian Timur Laut sebelah barat Sumatera. Penelitian ini menggunakan gabungan data citra NOAA-AVHRR dan MODIS untuk SPL, data citra SeaWiFS dan MODIS untuk klorofil-a, data angin permukaan bulanan diperoleh dari European Centre for Medium-Range Weather Forecasts (ECMWF). Data pendukung berupa indeks El Nino Southern Oscillation (ENSO) bulanan diperoleh dari laman https://www.ncdc.noaa.gov/teleconnections/ enso/indicators/ soi/ dan Dipole Mode Index (DMI) bulanan diperoleh dari laman https://www. jamstec.go.jp/virtualearth/general/en/index.html. Hasil penelitian menunjukkan bahwa SPL di daerah penelitian selama 22 tahun (1997–2019) berada pada kisaran 29,30 °C–31,60 °C dengan rata-rata 29,35 °C. Nilai SPL yang lebih tinggi terjadi saat Musim Barat sampai Musim Peralihan-1, sementara nilai yang lebih rendah pada Musim Timur sampai Musim Peralihan-2. Variabilitas nilai SPL dipengaruhi oleh pola angin musiman, intensitas radiasi matahari, dan Indian Ocean Dipole Mode (IODM). Saat IOD Negatif menyebabkan nilai SPL yang lebih tinggi dan konsentrasi Chl-a lebih rendah dari biasanya. Konsentrasi klorofil-a selama 22 tahun berkisar antara 0,0757 mg/m3–1,3006 mg/m3, konsentrasi klorofil-a yang lebih tinggi terjadi saat akhir Musim Timur (Agustus) dan awal Musim Barat (Desember), sementara nilai yang lebih rendah saat Musim Peralihan-1. Tingginya SPL berkisar pada Musim Peralihan-1 (Maret–Mei) bersamaan dengan rendahnya Chl-a pada musim yang sama diduga akibat terjadinya fenomena IOD negatif. Variabilitas Chl-a dipengaruhi oleh pola angin musiman, pergerakan massa air, dan IOD. Secara spasial konsentrasi Chl-a lebih tinggi didaerah pesisir dibandingkan di lepas pantai. Fenomena IOD mempengaruhi pola variasi interannual SPL dan konsentrasi Chl-a., Sea Surface Temperature (SST) and chlorophyll-a concentration are important parameters in waters that have an influence on oceanographic phenomena and oceanic productivity. The objective of this study was to analyze the variability of SST and chlorophyll-a concentration in the Northeast Indian Ocean off the West of Sumatra. The study used a combination of NOAA-AVHRR and MODIS image data for SST, SeaWiFS and MODIS image data for chlorophyll-a concenration, monthly surface wind data from the European Center for Medium Range Weather Forecasts (ECMWF). Supporting Data such as the monthly El Nino Southern Oscillation (ENSO) index and the Dipole Mode Index (DMI) were obtained from the web page of https://www.ncdc.noaa.gov/teleconnections/enso/ indicators/soi/ and https://www.jamstec.go.jp/virtualearth/general/en/index.html, respectively. The results showed that the range of SST during a 22 year period (1997–2019) was 29,30 °C–31,60 °C with the average of 29,35 °C where the higher SST occurred during the West Season and Transition Season 1, while the lower values were found during the East Season and Transition Season 2. variability of the SST values was related to the influence of seasonal winds, the intensity of solar radiation, and Indian Ocean Dipole Mode (IODM). When Negative IOD causing higher SST and lower Chl-a concentration than normal. Chlorophyll-a concentration for a 22 year perioed ranged of 0,0757-1,3006 mg/m3 where higher chlorophyll-a concentration occurred from the end of East Season (August) to the early of West Season (December), while lower values were found during Transition Season 1. The evidence of higher
Keyword: ENSO, IODM, Chlorophyll-a, Sea Surface Temperature

Judul: Metoda intramedullary pin sebagai salah satu cara menanggulangi fraktur femoralis pada anjing
Abstrak: Metoda intramedullary pin merupakan salah satu metoda penanggulangan fraktur yang populer karena banyak mempunyai keuntungan, diantaranya adalah : cepat dan mudah dikerja- kan, fiksasi yang dihasilkan lebih kuat dibandingkan metoda plate, setelah sembuh tulang menjadi lebih kuat, dan biaya yang digunakan relatif lebih ekonomis. Beberapa macam intramedullary pin yang ada, diantara- Steinmann pin, Rush pin, Kirschner pin, Kuentscher nya : nail, dan Leighton Shuttle pin. Teknik pemasangan intramedullary pin dapat melalui operasi tertutup atau operasi terbuka, tergantung dari ti- pe dan derajat fraktur. Pada operasi tertutup tidak dila- kukan pembukaan terhadap lokasi fraktur. Penyisipan pin dilakukan melalui fragmen fraktur proximal diteruskan ke fragmen distal, sehingga pada metoda ini luka yang timbul hanya pada tempat dimana pin tersebut dimasukkan. Pada operasi terbuka penyisipan pin dilakukan melalui pembukaan lokasi fraktur. Dalam melakukan pembukaan terhadap lokasi fraktur, harus dipilih pendekatan yang paling sesuai dan paling sedikit kemungkinannya untuk menimbulkan komplikasi. Pengambilan pin biasanya dilakukan setelah empat atau lima minggu disisipkan, diharapkan pada waktu itu telah terjadi pembentukan callus yang sudah cukup kuat untuk me- nunjang berdirinya tubuh. Pada beberapa keadaan pin tidak perlu diambil, misalnya pada anjing tua atau pada anjing yang menderita penyakit tulang. Tidak ada reaksi sakit... akibat pin bertahan di dalam tulang.
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