Kode Mata Kuliah | SB6117 / 4 SKS |
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Penyelenggara | 224 - Earth Sciences / FITB |
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Kategori | Lecture |
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| Bahasa Indonesia | English |
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Nama Mata Kuliah | Pemodelan Oseanografi Lanjut | Advanced Oceanographic Modelling |
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Bahan Kajian | - Pendahuluan: pemodelan pesisir dan laut
- Pemodelan numerik untuk sirkulasi fjord (1): Persamaan pembangun untuk sirkulasi fjord dan boundary condition – konstruksi algoritma numerik
- Pemodelan numerik untuk sirkulasi fjord (2):- Formula numerik untuk boundary condition – metoda untuk memperbaiki keakuratan – Memperbaiki keakuratan dan stabilitas dari persamaan frictional-diffusive-
- Pergerakan 3D di perairan dangkal (1):- Skema numerik orde ke 2
- Pergerakan 3D di perairan dangkal (2): Pendekatan diferensial orde ke-3
- Pemodelan 3D dengan menggunakan mode pemecahan dan koordinat sigma (1): pendekatan pemecahan rudiments
- Pemodelan 3D dengan menggunakan mode pemecahan dan koordinat sigma (2):- Solusi numerik dan implementasinya dari metoda pemecahan – transformasi koordinat sigma
- Koordinat sigma untuk model regional dan pesisir (1) Pendahuluan – persamaan pembangun - Vertical Mixing - Boundary Conditions - Mode Splitting
- Koordinat sigma untuk model regional dan pesisir (2) -numerik – arah vertical -arah horizontal -problem numerik -aplikasi -struktur kode
- Menjalankan program model sesuai kebutuhan masing-masing
- Simulasi arus 3D pada suatu kanal ideal (kedalaman uniform), pembangkit angin: Barotropik
- Simulasi arus 3D pada suatu kanal ideal (kedalaman uniform), pembangkit angin: Baroklinik (upwelling & downwelling)
| - Introduction: Coastal and Marine Modeling
- Numerical Modeling for Fjord Circulation (1): Formulation of Equations for Fjord Circulation and Boundary Conditions - Construction of Numerical Algorithm
- Numerical Modeling for Fjord Circulation (2):
Numerical Formulation for Boundary Conditions
Methods to Improve Accuracy
Improving Accuracy and Stability of Frictional-Diffusive Equations
- 3D Motion in Shallow Waters (1):
Second Order Numerical Scheme
- 3D Motion in Shallow Waters (2): Third Order Differential Approach
- 3D Modeling Using Split Mode and Sigma Coordinates (1): Basic Splitting Approach
- 3D Modeling Using Split Mode and Sigma Coordinates (2):
Numerical Solution and Implementation of Splitting Methods
Transformation of Sigma Coordinates
- Sigma Coordinates for Regional and Coastal Models (1):
Introduction
Formulation of Equations
Vertical Mixing
Boundary Conditions
Mode Splitting
- Sigma Coordinates for Regional and Coastal Models (2):
Numerical Methods
Vertical Direction
Horizontal Direction
Numerical Issues
Applications
Code Structure
- Running the Model Program as Needed
- 3D Current Simulation in an Ideal Channel (Uniform Depth), Wind Forcing: Barotropic
- 3D Current Simulation in an Ideal Channel (Uniform Depth), Wind Forcing: Baroclinic (Upwelling & Downwelling)
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Capaian Pembelajaran Mata Kuliah (CPMK) | - Memiliki kemampuan untuk menerapkan program model untuk contoh kasus yang sebenarnya.
| - Capable of applying model programs to real-world case studies.
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Metode Pembelajaran | Knowledge Based Leaning (KBL), Skill Based Learning (SBL), Problem based learning (PBL), Case-based Learning (CBL). | Knowledge Based Leaning (KBL), Skill Based Learning (SBL), Problem based learning (PBL), Case-based Learning (CBL). |
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Modalitas Pembelajaran | Luring, Sinkron, Asinkron | Offline, Synchronous, Asynchronous |
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Jenis Nilai | ABCDE |
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Metode Penilaian | Presentasi, Debat, Laporan, Praktik , UTS, UAS dan Tugas | Presentations, Debates, Reports, Practices, UTS, UAS and Assignments |
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Catatan Tambahan | Kuliah daring memungkinkan jika banyak hari libur nasional | Online classes are feasible if there are many public holidays |
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