Publications by authors named "Sherin C K"

This study examined the effects of solar light driven plastic degradation on carbon chemistry in the coastal waters of eastern Arabian Sea along the west coast of India. The research was conducted through experimental incubations exposed to natural sunlight at multiple locations between December 2023-February 2024. Photodegradation induced a significant pH decrease (up to 0.

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Article Synopsis
  • The study investigates how phytoplankton size classes (PSCs) respond to seasonal changes and coastal upwelling phases in the northern Indian Ocean, focusing on the southwestern coast of India.
  • During pre-upwelling, phytoplankton biomass is low with pico-PSCs dominating due to nutrient depletion, while early upwelling sees a shift to dominant micro-PSCs.
  • Peak upwelling leads to nutrient-rich conditions, enhancing larger micro- and meso-PSCs, and as nutrient enrichment declines in the later phases, nano- and pico-PSCs regain prominence, highlighting a clear transition in PSCs across different upwelling phases.
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Phytoplankton size classes (PSCs) are important in marine ecosystems because they organise the food chain and trophic pathways, which determine the overall biological environment. Based on three FORV Sagar Sampada cruises, the current study provides changes in PSCs in the Northeastern Arabian Sea (NEAS; north of 18 N) during different phases of the Northeast Monsoon [NEM (November-February)]. During all three phases of NEM such as early (November), peak (December), and late (February), in-situ chlorophyll-a fractionation data revealed that nanoplankton (2-20 μm) predominated, followed by microplankton (>20 μm) and picoplankton (0.

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Particulate organic carbon (POC) and its variability were studied to assess the accuracy of ocean colour retrieval algorithms over the eastern Arabian Sea (EAS) as it controls the carbon sequestration, oxygen minimum zone and biogeochemical (C, N and P) cycles. The seasonality in the physical and biological processes strongly influenced the distribution of POC along the EAS. Higher POC and chlorophyll a (chl a) during the spring inter monsoon (SIM) in the north EAS were due to detrainment bloom.

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