IIOSC - 2025

IIOSC - 2025

International Indian Ocean Science Conference - 2025

Celebrating 10 years of the Second International Indian Ocean Expedition

01-05 December 2025
INCOIS, Hyderabad, India.

Summary of Abstract Submission



Abstract Submission No.ABS-04-0263
Title of AbstractIMPACT OF CLIMATE VARIABILITY ON PHYTOPLANKTON DYNAMICS IN THE INDIAN OCEAN
AuthorsHaritha M*, Abhinav Gummalla, Dr. PV Nagamani, Anju Kumari
OrganisationNational Remote Sensing Centre- Hyderabad, CUSAT
AddressManazhithodi (House), Kunnakkavu post, Malappuram, 679340
Perinthalmanna, Kerala, India
Pincode: 679340
E-mail: haridasharitha1996@gmail.com
CountryIndia
PresentationOral
AbstractThe Indian Ocean basin, particularly its western sector, is among the most biologically productive tropical ocean regions, driven by strong monsoon dynamics and basin-scale mesoscale processes. However, this productivity is increasingly threatened by rapid surface warming, which has reduced phytoplankton abundance by up to 20% in recent decades. To better understand the climate controls on biological variability, we analyzed two decades (2000⿿2024) of satellite-derived chlorophyll a (Chl-a), sea surface temperature (SST), and sea level anomaly (SLA) data, focusing on the influence of the Indian Ocean Dipole (IOD) and El Niño⿿Southern Oscillation (ENSO). Time series and Hovmöller analyses highlight substantial seasonal and interannual Chl-a variability, particularly in the western Indian Ocean during the summer monsoon. Cross-correlation and variance decomposition reveal that, over the long term, both ENSO and IOD significantly modulate productivity, but their relative roles have shifted. ENSO emerged as the dominant driver across most basins, explaining up to 75⿿80% of Chl-a variance in 2023 (e.g., Somali and Mascarene basins). In contrast, the IOD⿿s contribution weakened markedly (from 33.4% to 6.6% in the Central Indian Ocean), though it remained influential in the Bay of Bengal. A high positive ENSO⿿IOD correlation in 2023 (r = 0.94) amplified shared climatic forcing, altered lead⿿lag relationships, and intensified chlorophyll variability beyond the effect of either mode alone. Our findings underscore that analyzing long-term Chl-a variability while characterizing ENSO⿿IOD interactions at basin and regional scales strengthens understanding of how climate-driven physical processes regulate phytoplankton dynamics. This integrative perspective is critical for forecasting ecosystem responses and guiding sustainable marine resource management under accelerating climate variability and change.
Are you part of IIOE-2 endorsed projectno
KeywordsOcean productivity, Climate change, IOD, ENSO, Ocean Physical processes, SLA, SST
For Awardsyes
Date Of Birth18-11-1996
ECSN Registration NumberIIOE2-ECSN-0252