STASIUN METEOROLOGI MARITIM

KEDUDUKAN DAN TUGAS

Organisasi Stasiun Meteorologi Maritim ditetapkan dengan Keputusan Kepala Badan Meteorologi dan Geofisika Nomor : KEP 005 Tahun 2004 tanggal 5 Oktober 2004

Stasiun Meteorologi Maritim mempunyai tugas melaksanakan pengamatan, pengumpulan dan penyebaran data, pengolahan, analisis dan prakiraan didalam wilayahnya serta pelayanan jasa meteorologI

Selaku Port Meteorological Office (PMO) juga melakukan tugas :

• Pemeriksaan peralatan pengamatan meteorologi atas dasar permintaan nakhoda kapal serta memberikan beberapa petunjuk dan saran dalam masalah kecuacaan
  
• Memelihara kontak dengan petugas pengamat cuaca di kapal serta melakukan pemeriksaan/ inspeksi peralatan pengamat cuaca yang terdapat di kapal
  
• Memelihara hubungan baik dengan para pemilik kapal maupun agen kapal, dari berbagai kebangsaan, dengan tujuan mengadakan kerjasama dengan kapal ataupun dalam rangka lebih menggiatkan pengamatan cuaca di laut.
  

 

JUMLAH STASIUN

Stasiun Meteorologi Maritim ada 10 (sepuluh) :

1. Stasiun Meteorologi Maritim Belawan

2. Stasiun Meteorologi Maritim Teluk Bayur

3. Stasiun Meteorologi Maritim Panjang Lampung

4. Stasiun Meteorologi Maritim Tanjung Priok

5. Stasiun Meteorologi Maritim Semarang

6. Stasiun Meteorologi Maritim Surabaya

7. Stasiun Meteorologi Maritim Pontianak

8. Stasiun Meteorologi Maritim Paotere Makassar

9. Stasiun Meteorologi Maritim Kendari

10. Stasiun Meteorologi Maritim Bitung

KEGIATAN STASIUN

OBSERVASI

Pengamatan konvensional

Pengamatan Automatic (AWS)

Komunikasi : Pengumpulan/ penyebaran data, informasi cuaca dan gelombang melalui Computer Message Switching System (CMSS), Internet, Faximile, Telepon

Peralatan teknis : memelihara/ memperbaiki peralatan , pengecekan peralatan meteo di kapal dan di Stasiun.

 

DATA DAN INFORMASI

Pengolahan Data : Klimat, Data dari alat AWS, Ploting data synop dan pibal.

Akses data satelit via internet

Analisa Peta Synoptic

Membuat Prakiraan Cuaca dan Gelombang

Pelayanan Jasa Meteorologi

PORT METEOROLOGICAL OFFICE (PMO)

Kunjungan ke kapal-kapal

Ikut serta berlayar (Family Voyage)

PRODUK JASA METEOROLOGI MARITIM

Data Klimatologi

Data hasil pengamatan AWS

Weather Bulletin for Shipping

Informasi Cuaca Pelayaran

Prakiraan Cuaca dan Gelombang di Pelabuhan

Analisis/ Prakiraan Gelombang, Arus laut, Upweling mengunakan program Windwaves-05

DAFTAR ALAMAT, TELEPON, TELEFAC DAN EMAIL

NO.	KANTOR	TELEPON	TELEFAX	E' MAIL	ALAMAT KANTOR
1	STAMET MARITIM TANJUNG PRIOK	021 43901650, 021 4351366	021 43930339	martpk04@yahoo.com mar_tpk@jakarta.wasantara.net.id	Jln. Padamarang no. 4A Pelabuhan Tanjung Priok , Jakarta Utara 14310
2	STAMET MARITIM BELAWAN	061 6840340	061 6841851	stamar_blw@hotmail.com	Jln. Raya Pelabuhan III Gabion Ringkai Begawan-Medan
3	STAMET MARITIM TELUK BAYUR	0751 62331	0751 62331	meteomaritim_tlbayur@yahoo.co.id	Jln. Cilacap No. 31A Padang 25217
4	STAMET MARITIM PANJANG LAMPUNG	0721 342219	0721 257711	stamarpjg@yahoo.com	Jln. Djawa No. 12 Pelabuhan Panjang Bandar Lampung
5	STAMET MARITIM SEMARANG	024 3559194	024 3549050	sta_mar2@hotmail.com	Jln. Deli no. 3 Pelabuhan Emas Semarang
6	STAMET MARITIM PONTIANAK	0561 769906	0561 769906	tejomaritim06@yahoo.com	Jln. Pelabuhan Dwikora (komplek pelabuhan laut) Pontianak
7	STAMET MARITIM SURABAYA	031 3291439	031 3291439	meteomaritmsby@yahoo.co.id	Jln. Kalimas Baru 97B Perak Surabaya
8	STAMET MARITIM MAKASSAR	0411 319242	0411 328235	meteo_marptr@yahoo.co.id	Jln. Sabutung I no. 30 Paotere Makassar
9	STAMET MARITIM BITUNG	0438 21710	0438 21710	stamarbitung@yahoo.com	Jln. Candi no. 56 Kaduodan Bitung
10	STAMET MARITIM KENDARI	0401 328528	0401 328528	stamarkdi@plasa.com	Jln. Jenderal Sudiramn no. 158 Kendari 93127
11	STA METEOROLOGI CILACAP	0282 534103	0282 534103	yoyoid2002@yahoo.com	Jln. Gatot Subroto no. 20 Cilacap
12	STA METEOROLOGI BIAK	0981 21284	0981 22824	dukuncuaca@yahoo.co.id	Jln. Prof. Moch Yamin Biak
13	STA METEOROLOGI KUPANG	0380 881613	0380 882097	met_kupang@yahoo.com	Jln. Rajawali Penturi Kupang

 

Ocean wave

Ocean surface waves are the result of forces acting on the ocean. The predominant natural forces are pressure or stress from the atmosphere (especially through the winds), earthquakes, gravity of the Earth and celestial bodies (the Moon and Sun), the Coriolis force (due to the Earth's rotation) and surface tension. The characteristics of the waves depend on the controlling forces. Tidal waves are generated by the response to gravity of the Moon and Sun and are rather large-scale waves. Capillary waves, at the other end of the scale, are dominated by surface tension in the water. Where the Earth's gravity and the buoyancy of the water are the major determining factors we have the so-called gravity waves.

Waves may be characterized by their period. This is the time taken by successive wave crests to pass a fixed point. The type and scale of forces acting to create the wave are usually reflected in the period. Figure 1.1 illustrates such a classification of waves.

On large scales, the ordinary tides are ever present but predictable. Less predictable are tsunamis (generated by earthquakes or land movements), which can be catastrophic, and storm surges. The latter are associated with the movement of synoptic or meso-scale atmospheric features and may cause coastal flooding.

Wind-generated gravity waves are almost always present at sea. These waves are generated by winds somewhere on the ocean, be it locally or thousands of kilometres away. They affect a wide range of activities such as shipping, fishing, recreation, coastal and offshore industry, coastal management (defences) and pollution control. They are also very important in the climate processes as they play a large role in exchanges of heat, energy, gases and particles between the oceans and atmosphere. It is these waves which will be our subject in this Guide.

To analyse and predict such waves we need to have a model for them, that is we need to have a theory for how they behave. If we observe the ocean surface we note that the waves often form a rather complex pattern. To begin we will seek a simple starting model, which is consistent with the known dynamics of the ocean surface, and from this we will derive a more complete picture of the wind waves we observe.

The model of the ocean which we use to develop this picture is based on a few quite simple assumptions: • The incompressibility of the water. This means that the density is constant and hence we can derive a continuity equation for the fluid, expressing the conservation of fluid within a small cell of water (called a water particle); • The inviscid nature of the water. This means that the only forces acting on a water particle are gravity and pressure (which acts perpendicular to the surface of the water particle). Friction is ignored; • The fluid flow is irrotational. This means that the individual particles do not rotate. They may move around each other, but there is no twisting action. This allows us to relate the motions of neighbouring particles by defining a scalar quantity, called the velocity potential, for the fluid. The fluid velocity is determined from spatial variations of this quantity.

From these assumptions some equations may be written describe the motion of the fluid