Kenaikan muka air laut (sea level rise) merupakan konsekuensi dari perubahan iklim yang memiliki dampak signifikan terhadap kehidupan sosial, ekonomi, dan infrastruktur, serta ancaman tenggelamnya kawasan pesisir Indonesia yang ditinggali oleh 60% penduduknya. Sejak akhir abad ke-19, perubahan kedudukan air laut diamati dari stasiun pasang surut di sepanjang garis pantai. Namun, pengamatan stasiun pasang surut memiliki keterbatasan dalam jumlah, distribusi, dan jangkauannya, serta adanya pengaruh land subsidence. Oleh karena itu, penelitian ini menganalisis tren kenaikan muka air laut Indonesia menggunakan data pengamatan misi referensi satelit altimetri, yaitu Topex/Poseidon, Jason 1, Jason 2, dan Jason 3. Setelah dilakukan least square intercalibrated dan a-seasonal-trend decomposition procedure based on loess diketahui bahwa laju sea level rise di Indonesia +4,5 mm/tahun pada periode tahun 1993-2018. Tren linier bernilai positif ini menunjukkan bahwa ketinggian muka laut di Indonesia akan terus meningkat dengan persamaan y = 4,6x-9133,5 mm, dimana y adalah sea level anomaly dan x adalah waktu. Sehingga berdasarkan hasil tersebut dapat dilakukan perencanaan pra-kejadian terhadap dampak dari sea level rise yang akan mendatang.
The Global Navigation Satellite System (GNSS), nowadays, is to be an important tool for determining positions and times on the real-time and post-processing applications. This study aims to assess the performance of the single frequency L1-GPS using low cost receivers. The performance will be evaluated by comparing with the geodetic L1+L2 GPS receiver to positioning performance. The low cost receivers used were Ublox NEO-M8T and Allystar HD9100. While, the dual frequency GPS TOPCON was used as reference receiver. The results show, RTK mode can improve the accuracy compare with single positioning up to centimetres. In this experiment, the Allystar HD9100 gives a better result than Ublox Neo M8T. However, the result discrepancies may be caused by the simple antenna splitter.
Sea-level rise is a big problem in the future. Indonesia is a country with the potential impacts of sea-level rise; therefore, the continuous monitoring of sea-level variability becomes urgent. Globally, sea-level rise is up to 3 mm year−1 estimated by satellite altimetry data. How about the sea level rise in Indonesia, particularly in western Indonesia such as Java sea, Karimata Strait? This paper aims to estimate the sea-level rise in the western Indonesian seas, such as the Java Sea and the Karimata Strait. The estimation was derived using the Cryosat-2 altimetry data. The data used is in a period of 9 years (2010 to 2018). The trend in the period is negative 4 mm year−1. The area also has a low correlation with ENSO with a value negative 0.25
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