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dc.contributor.authorJyothibabu, R.
dc.contributor.authorKarnan, C.
dc.contributor.authorArunpandi, N.
dc.contributor.authorSanthiKrishnan, S.
dc.contributor.authorBalachandran, K.K.
dc.contributor.authorSahu, K.C.
dc.date.accessioned2021-01-31
dc.date.accessioned2021-02-09T10:13:09Z
dc.date.available2021-01-01
dc.date.available2021-02-09T10:13:09Z
dc.date.issued2021
dc.identifier.citationEcological Indicators, vol.121; 2021; Article no: 107016
dc.identifier.issn1470-160X
dc.identifier.otherhttps://www.sciencedirect.com/science/article/abs/pii/S1470160X20309559
dc.identifier.urihttps://doi.org/10.1016/j.ecolind.2020.107016
dc.identifier.urihttp://drs.nio.org/drs/handle/2264/8360
dc.descriptionIF2019 - 4.229
dc.description.abstractThis paper introduces the cumulative impact of cyclonic (cold-core) and anticyclonic (warm-core) eddies on the distribution of phytoplankton biomass in the Bay of Bengal (BoB). Estimations of the ocean surface eddy features in the BoB using satellite-derived monthly, seasonal, and multi-year (2012-2016) datasets showed significant dominance of warm-core features over the cold-core ones. Multi-year monthly data of the BoB evidenced strikingly higher geographical area (%) for warm cores (av. 16.5 ± 5.5) compared to the cold-core features (av. 2 ± 1.2). The highest warm-core extent (%) was in May (av. 25.8 ± 1.4), followed by April (av. 22.6 ± 1.4), February (av. 19.5 ± 0.3) and March (av. 18.3 ± 0.9). Contrastingly, a relatively higher extent (%) of cold cores occurred in November (av. 3.9 ± 2.2), October (av. 3.78 ± 2.0), and December (av. 3.5 ± 2.1). The analysis also showed that the extreme oligotrophy of the study domain during the Pre-Monsoon (March-May) was caused by a robust, warm gyre. Upwelling and winter convection, which enhances phytoplankton biomass in the Arabian Sea, are either very weak or absent in the BoB. Similarly, nutrient inputs through river influx into the BoB are insufficient to enhance phytoplankton stock beyond the shelf waters. In this scenario, we showed here that the significantly larger spread of warm-core over the cold-core eddies is a simple ecological indicator of the basin-scale low phytoplankton stock in the BoB.
dc.languageen
dc.publisherElsevier B.V.
dc.relation.ispartofEcol Indic
dc.relation.isreferencedbySCI
dc.rightsOnly the author version of the copright reserved papers uploaded. Contact drs@nio.org for any complaints regarding copyright violations
dc.titleSignificantly dominant warm-core eddies: An ecological indicator of the basin-scale low biological production in the Bay of Bengal
dc.typeJournal Article
dc.affiliation.authorCSIR-National Institute of Oceanography, Kochi, Kerala, India


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