Role of interannual equatorial forcing on the subsurface temperature dipole in the Bay of Bengal during IOD and ENSO events
Role of interannual equatorial forcing on the subsurface temperature dipole in the Bay of Bengal during IOD and ENSO events
Role of equatorial forcing on the thermocline variability in the Bay of Bengal (BoB) during positive and negative phases of the Indian Ocean Dipole (IOD) and El Niño Southern Oscillation (ENSO) was investigated using the Regional Ocean Modeling System (ROMS) simulations during 1988 to 2015. Two numerical experiments were carried out for (i) the Indian Ocean Model (IOM) with interannual open boundary conditions and (ii) the BoB Model (BoBM) with climatological boundary conditions. The first mode of Sea Surface Height Anomalies (SSHA) variability showed a west-east dipole nature in both IOM and altimetry observations around 11°N, which was absent in the BoBM. The vertical section of temperature along the same latitude showed a sharp subsurface temperature dipole with a core at ~ 100 m depth. The positive (negative) subsurface temperature anomalies were observed over the whole northeastern BoB during NIOD (PIOD) and LN (EN) composites due to stronger (weaker) second downwelling Kelvin Waves. During the negative phases of IOD and ENSO, the cyclonic eddy on the southwestern BoB strengthened due to intensified southward coastal current along the western BoB and local wind stress. The subsurface temperature dipole was at its peak during October–December (OND) with 1-month lag from IOD and was evident from the Argo observations and other reanalysis datasets as well. A new BoB dipole index (BDI) was defined as the normalized difference of 100-m temperature anomaly and found to be closely related to the frequency of cyclones and the surface chlorophyll-a concentration in the BoB.
1253–1271
Pramanik, Saikat
dec4ec8d-a488-48c3-b2dc-ae9181e9d1bc
Sil, Sourav
848193f4-a406-462f-b184-f1f2f5098f93
Mandal, Samiran
52e3ff2f-e131-411b-a2de-f32a170494bb
Dey, Dipanjan
6abca563-f99d-4554-a0b8-945d5621b16b
Shee, Abhijit
85ace301-7c49-42a9-967a-a6257afd2d29
4 November 2019
Pramanik, Saikat
dec4ec8d-a488-48c3-b2dc-ae9181e9d1bc
Sil, Sourav
848193f4-a406-462f-b184-f1f2f5098f93
Mandal, Samiran
52e3ff2f-e131-411b-a2de-f32a170494bb
Dey, Dipanjan
6abca563-f99d-4554-a0b8-945d5621b16b
Shee, Abhijit
85ace301-7c49-42a9-967a-a6257afd2d29
Pramanik, Saikat, Sil, Sourav, Mandal, Samiran, Dey, Dipanjan and Shee, Abhijit
(2019)
Role of interannual equatorial forcing on the subsurface temperature dipole in the Bay of Bengal during IOD and ENSO events.
Ocean Dynamics, .
(doi:10.1007/s10236-019-01303-0).
Abstract
Role of equatorial forcing on the thermocline variability in the Bay of Bengal (BoB) during positive and negative phases of the Indian Ocean Dipole (IOD) and El Niño Southern Oscillation (ENSO) was investigated using the Regional Ocean Modeling System (ROMS) simulations during 1988 to 2015. Two numerical experiments were carried out for (i) the Indian Ocean Model (IOM) with interannual open boundary conditions and (ii) the BoB Model (BoBM) with climatological boundary conditions. The first mode of Sea Surface Height Anomalies (SSHA) variability showed a west-east dipole nature in both IOM and altimetry observations around 11°N, which was absent in the BoBM. The vertical section of temperature along the same latitude showed a sharp subsurface temperature dipole with a core at ~ 100 m depth. The positive (negative) subsurface temperature anomalies were observed over the whole northeastern BoB during NIOD (PIOD) and LN (EN) composites due to stronger (weaker) second downwelling Kelvin Waves. During the negative phases of IOD and ENSO, the cyclonic eddy on the southwestern BoB strengthened due to intensified southward coastal current along the western BoB and local wind stress. The subsurface temperature dipole was at its peak during October–December (OND) with 1-month lag from IOD and was evident from the Argo observations and other reanalysis datasets as well. A new BoB dipole index (BDI) was defined as the normalized difference of 100-m temperature anomaly and found to be closely related to the frequency of cyclones and the surface chlorophyll-a concentration in the BoB.
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Accepted/In Press date: 23 August 2019
Published date: 4 November 2019
Identifiers
Local EPrints ID: 457034
URI: http://eprints.soton.ac.uk/id/eprint/457034
ISSN: 1616-7341
PURE UUID: 227692c5-4d69-435b-a588-d0fc8b8b1643
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Date deposited: 19 May 2022 16:56
Last modified: 17 Mar 2024 04:12
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Author:
Saikat Pramanik
Author:
Sourav Sil
Author:
Samiran Mandal
Author:
Abhijit Shee
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