Please use this identifier to cite or link to this item: http://hdl.handle.net/10603/478096
Title: Biophysical coupling Chlorophyll a dynamics of the North Eastern Arabian Sea in a warming scenari
Researcher: Hussain, Midhun Shah
Guide(s): Mohamed Hatha, A A and Smitha, B R
Keywords: Fluid Dynamics
Life Sciences
Marine and Freshwater Biology
Phytoplankton Classification
Plant and Animal Science
Surface subsurface oscillations - Chlorophyll
University: Cochin University of Science and Technology
Completed Date: 2022
Abstract: newlineThe thesis address the role of physical drivers such as temperature, density, newlinemixing/stratification, settling velocity, and light in defining the vertical structure newlineof Chlorophyll (Chl-a) and the phytoplankton in the upper layers of the North newlineEastern Arabian Sea (NEAS). The study utilized a wide range of data from newlineBio-Argo (250 profiles from 4 floats, employing appropriate validation exercises newlineand processed/analyzed using self-developed tool Ponman), remote sensing newlinesatellites, and CTD profiles collected during the period 2003 to 2019. The newlinecrux of the study is oriented about the Gaussian characteristics of the Chl-a newlineprofile and the Stokes relation in fluid dynamics to explain Settling depth and newlinevelocity. The Principle Component Analysis (PCA) illustrates the dominant newlinerole of density( t) and its gradient over Photosynthetically Active Radiation newline(PAR). The study found significant relation of Subsurface Chlorophyll Maxima newline(SCM) with the buoyancy frequency, especially during the stratified spring newlineconditions (February-March). This change is reflected well in the settling newlinesimulations, which attempted on the ten regionally dominant species. The SCM newlineis well prominent after every bloom, and as reflected in the surface-subsurface newlineinteractions evinced in the Dynamic Time Wraps (DTW), Noctiluca scintillans newlinesubstantially contribute to the SCM. Winter-driven convective mixing and the newlinespring settling result in the ascending and descending phytoplankton in the newlinewater column. The Empirical Orthogonal Teleconnections (EOTs) show that newlinethese oscillations locally do control by the prevailing currents and mesoscale newlineprocesses like eddies. The Lotka-Volterra Model (LVM) suggests strong trophic newlinerelations between the dominant prey (diatom) and predator (Noctiluca) during newlinewinter-spring
Pagination: 246
URI: http://hdl.handle.net/10603/478096
Appears in Departments:Department of Marine Biology, Microbiolgy and Biochemistry

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02_preliminary pages.pdf572.25 kBAdobe PDFView/Open
03_content.pdf233.68 kBAdobe PDFView/Open
04_abstract.pdf179.19 kBAdobe PDFView/Open
05_chapter1.pdf7.39 MBAdobe PDFView/Open
06_chapter2.pdf2.09 MBAdobe PDFView/Open
07_chapter3.pdf9.06 MBAdobe PDFView/Open
08_chapter4_.pdf372.85 kBAdobe PDFView/Open
09_chapter5.pdf21.49 MBAdobe PDFView/Open
10_chapter6.pdf5.11 MBAdobe PDFView/Open
11_chapter7.pdf339.66 kBAdobe PDFView/Open
14_annexures.pdf3.98 MBAdobe PDFView/Open
80_recommendation.pdf453.86 kBAdobe PDFView/Open
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