Open AccessLow-Frequency Currents from Deep Moorings in the Southern Bay of Bengal
Author(s) -
H. W. Wijesekera,
William J. Teague,
D. W. Wang,
Ewa Jarosz,
Tommy G. Jensen,
S.U.P. Jinadasa,
Harindra J. S. Fernando,
Zachariah R. Hallock
Publication year - 2016
Publication title -
journal of physical oceanography
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.706
H-Index - 143
eISSN - 1520-0485
pISSN - 0022-3670
DOI - 10.1175/jpo-d-16-0113.1
Subject(s) - eddy , bay , anticyclone , hydrography , oceanography , geology , monsoon , bengal , physical oceanography , hydrographic survey , boundary current , ocean current , temperature salinity diagrams , climatology , current meter , mooring , current (fluid) , salinity , meteorology , geography , turbulence
High-resolution currents and hydrographic fields were measured at six deep-water moorings in the southern Bay of Bengal (BoB) by the Naval Research Laboratory as part of an international effort focused on the dynamics of the Indian Ocean. Currents, temperature, and salinity were sampled over the upper 500 m for 20 months between December 2013 and August 2015. One of the major goals is to understand the space–time scales of the currents and physical processes that contribute to the exchange of water between the BoB and the Arabian Sea. The observations captured Southwest and Northeast Monsoon Currents, seasonally varying large eddies including a cyclonic eddy, the Sri Lanka dome (SLD), and an anticyclonic eddy southeast of the SLD. The observations further showed intraseasonal oscillations with periods of 30–70 days, near-inertial currents, and tides. Monthly averaged velocities commonly exceeded 50 cm s −1 near the surface, and extreme velocities exceeded 150 cm s −1 during the southwest monsoon. Tides were small and dominated by the M 2 component with velocities of about 3 cm s −1 . The average transport into the BoB over the measurement period was 2 Sv (1 Sv ≡ 10 6 m 3 s −1 ) but likely exceeded 15 Sv during summer of 2014. This study suggests the water exchange away from coastal boundaries, in the interior of the BoB, may be largely influenced by the location and strength of the two eddies that modify the path of the Southwest Monsoon Current. In addition, there is a pathway below 200 m for transport of water into the BoB throughout the year.