The University of Southampton
University of Southampton Institutional Repository

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 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.
1616-7341
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
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, 1253–1271. (doi:10.1007/s10236-019-01303-0).

Record type: Article

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.

This record has no associated files available for download.

More information

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
ORCID for Dipanjan Dey: ORCID iD orcid.org/0000-0002-9588-4042

Catalogue record

Date deposited: 19 May 2022 16:56
Last modified: 17 Mar 2024 04:12

Export record

Altmetrics

Contributors

Author: Saikat Pramanik
Author: Sourav Sil
Author: Samiran Mandal
Author: Dipanjan Dey ORCID iD
Author: Abhijit Shee

Download statistics

Downloads from ePrints over the past year. Other digital versions may also be available to download e.g. from the publisher's website.

View more statistics

Atom RSS 1.0 RSS 2.0

Contact ePrints Soton: eprints@soton.ac.uk

ePrints Soton supports OAI 2.0 with a base URL of http://eprints.soton.ac.uk/cgi/oai2

This repository has been built using EPrints software, developed at the University of Southampton, but available to everyone to use.

We use cookies to ensure that we give you the best experience on our website. If you continue without changing your settings, we will assume that you are happy to receive cookies on the University of Southampton website.

×