| ชื่อเรื่อง | : | Equatorward western boundary current in the Bay of Bengal during November - December 1983 |
| นักวิจัย | : | Babu, M.T. |
| คำค้น | : | - |
| หน่วยงาน | : | National Institute Of Oceanography (NIO), India |
| ผู้ร่วมงาน | : | - |
| ปีพิมพ์ | : | 2535 |
| อ้างอิง | : | Physical processes in the Indian Seas. Proc. 1 Convention ISPSO, 1990. Ed. by: Swamy, G.N., 57-62p. , http://drs.nio.org/drs/handle/2264/3110 |
| ที่มา | : | - |
| ความเชี่ยวชาญ | : | - |
| ความสัมพันธ์ | : | - |
| ขอบเขตของเนื้อหา | : | - |
| บทคัดย่อ/คำอธิบาย | : | Geostrophic circulation derived from the observed hydrographic data for the period November-December (1983) indicates the presence of a strong equatorward western boundary current (WBC) in the Bay of Bengal. The curl sub(z) phi based on the climatological mean wind field for the same period brodly shows a negative field in the northern part which suggests a southward current away from the western boundary with an expected Munk layer flowing northward opposing. The WBC takes a turn and flows zonally eastward at about 12 degrees N where curlz is zero. Subsequently, a cold core gyre (CCG) is formed in the central Bay when the zonal flow merges with the northward current at 9 degrees C. It is concluded that the WBC is mainly driven by the cross-shore density gradients causEd. by large quantity of river run-off |
| บรรณานุกรม | : |
Babu, M.T. . (2535). Equatorward western boundary current in the Bay of Bengal during November - December 1983.
: National Institute Of Oceanography (NIO), India. Babu, M.T. . 2535. "Equatorward western boundary current in the Bay of Bengal during November - December 1983".
: National Institute Of Oceanography (NIO), India. Babu, M.T. . "Equatorward western boundary current in the Bay of Bengal during November - December 1983."
: National Institute Of Oceanography (NIO), India, 2535. Print. Babu, M.T. . Equatorward western boundary current in the Bay of Bengal during November - December 1983. : National Institute Of Oceanography (NIO), India; 2535.
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