Abstract

Arabian Sea is in general biologically most productive region in the North Indian Ocean, in particular eastern Arabian Sea. However, there is a lack of pre-existing studies performed to reveal the seasonal and interannual variability of the primary production. The potential role of atmospheric and oceanographic events on promoting the distinct development of phytoplankton in the northern and southern parts of eastern Arabian Sea regions was investigated in this article. In order to study the temporal variability of the bio-physical parameters, we used 12 years (1998-2009) of Sea WiFS chlorophyll-a data and 10 years (2000-2009) of QuickSCAT wind stress data (zonal and meridional) as two important forcing parameters. Relative impacts of the Indian Ocean Dipole (IOD), associated with the global climatic event of El Nino Southern Oscillation (ENSO) on biophysical parameters of eastern Arabian Sea during the study period have been analyzed at the two regions. Seasonal and interannual variabilities are clearly observed in both chlorophyll-a and wind stress time series. The overall seasonal variation for chlorophyll-a were 0.17 and 2.29 mg m-3 with a standard deviation of 0.03 and 0.54 mg m-3 for the northern and southern regions, respectively, and the coefficient of variation was 8-65%. The relationship between chlorophyll-a and multivariate ENSO index was negative at northern and southern regions in all seasons, and the IOD also showed negative relation except pre monsoon sea.

Highlights

  • Ocean is one of the main resources for the human and other species living on our planet Earth

  • In Arabian Sea it is expected that the interaction between the open-sea and the coastal regime is important to the dynamics of the Sea

  • The main objective of this study is to investigate the seasonal and inter-annual bio-physical changes in the eastern Arabian Sea especially at the southern and northern parts

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Summary

Introduction

The Arabian Sea is one of the most biologically active regions in the world. It is approximately triangular basin with largest zonal extent of about 3000 km and a slightly smaller meridional extent. The monsoonal wind system in summer and winter over the Arabian Sea drives spectacular seasonal variations, for example the annual reversal of the surface circulation. The Arabian Sea experiences extremes in atmospheric forcing which leads one of the largest intra-annual variability compared to the other ocean basins of the world. The semi-annual reversals in atmospheric and ocean circulation, the inflow of warm high saline waters from the Persian Gulf and the Red Sea, and the zone of oxygen deficient waters (~150-1000 m) make the Arabian Sea a unique tropical basin

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