• Influence of the extreme Indian Ocean dipole 2019 on the equatorial Indian Ocean circulation. 

  Gangiredla, S.; Amol, P.; Mukherjee, A. (Springer, 2024)

  This study examines direct current measurements in the central equatorial Indian Ocean during the positive phase of the extreme Indian Ocean Dipole (pIOD) in 2019. Analysis of near-surface zonal current at 77E and 83E ...

• Impact of the Pacific-Japan pattern on the tropical Indo-western Pacific Ocean surface waves 

  Gangiredla, S.; Remya, P.G.; Dey, S.P.; Chowdary, J. S.; Kumar, P. (Springer, 2024)

  The present study examines the impact of the Pacific-Japan (PJ) pattern on tropical Indo Western Pacific Ocean significant wave heights during the boreal summer season (June through August, JJA) for the first time. The PJ ...

• Distribution and sea-to-air fluxes of nitrous oxide and methane from a seasonally hypoxic coastal zone in the southeastern Arabian Sea 

  Arya, K.S.; Gireeshkumar, T.R.; Vignesh, E.R.; Muraleedharan, K.R.; DeCunha, M.S.; Emil, J.C.R.; Snigtha; Mariya, C.; Nair, C.R.; Praveena, S. (Elsevier, 2024)

  The seasonal variability, pathways, and sea-to-air fluxes of nitrous oxide (N2O) and methane (CH4) in the coastal environment, where coastal upwelling and mudbanks co-exist are presented based on the monthly time-series ...

• Plankton diversity and dynamics in the upper surface of the Indian sector of the Southern Ocean ecosystem and biogeochemical processes 

  Sreerag, A.; Mishra, R.K.; Naik, R.K.; Venkataramana, V.; Soares, M.A.; Mahale, R.; AnilKumar, N.; Gauns, M. (Elsevier, 2023)

  In the Southern Ocean (SO) marine ecosystem, the interplay between CO2 sink and climate change is closely linked to the shifting plankton communities, leading to potentially wide-ranging biogeochemical effects. Within the ...

• Behaviour of barium in the tropical estuaries: Implications to its marine budgets and paleo-oceanographic applications 

  Rahaman, W.; Singh, S.K. (Elsevier, 2023)

  Marine Barium (Ba) is extensively used as a tracer for biogeochemical processes and paleo-oceanographic proxy for past river discharge, salinity, and long-term hydrological changes. However, poor constrain on the riverine ...

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