eCite Digital Repository

Biogeochemical variability in the central equatorial Indian Ocean during the monsoon transition

Citation

Strutton, PG and Coles, VJ and Hood, RR and Matear, RJ and McPhaden, MJ and Phillips, HE, Biogeochemical variability in the central equatorial Indian Ocean during the monsoon transition, Biogeosciences, 12, (8) pp. 2367-2382. ISSN 1726-4170 (2015) [Refereed Article]


Preview
PDF
2Mb
  

Copyright Statement

Copyright 2014 The Authors-This article has been distributed under the terms of the Creative Commons Attribution License. (CC BY 3.0 AU)

Official URL: http://dx.doi.org/10.5194/bgd-11-6185-2014

DOI: doi:10.5194/bg-12-2367-2015

Abstract

In this paper we examine time-series measurements of near-surface chlorophyll concentration from a mooring that was deployed at 80.5°E on the equator in the Indian Ocean in 2010. These data reveal at least six striking spikes in chlorophyll from October through December, at approximately 2-week intervals, that coincide with the development of the fall Wyrtki jets during the transition between the summer and winter monsoons. Concurrent meteorological and in situ physical measurements from the mooring reveal that the chlorophyll pulses are associated with the intensification of eastward winds at the surface and eastward currents in the mixed layer. These observations are inconsistent with upwelling dynamics as they occur in the Atlantic and Pacific oceans, since eastward winds that force Wyrtki jet intensification should drive downwelling. The chlorophyll spikes could be explained by two alternative mechanisms: (1) turbulent entrainment of nutrients and/or chlorophyll from across the base of the mixed layer by wind stirring or Wyrtki jet-induced shear instability or (2) enhanced southward advection of high chlorophyll concentrations into the equatorial zone. The first mechanism is supported by the phasing and amplitude of the relationship between wind stress and chlorophyll, which suggests that the chlorophyll spikes are the result of turbulent entrainment driven by synoptic zonal wind events. The second mechanism is supported by the observation of eastward flows over the Chagos–Laccadive Ridge, generating high chlorophyll to the north of the equator. Occasional southward advection can then produce the chlorophyll spikes that are observed in the mooring record. Wind-forced biweekly mixed Rossby gravity waves are a ubiquitous feature of the ocean circulation in this region, and we examine the possibility that they may play a role in chlorophyll variability. Statistical analyses and results from the OFAM3 (Ocean Forecasting Australia Model, version 3) eddy-resolving model provide support for both mechanisms. However, the model does not reproduce the observed spikes in chlorophyll. Climatological satellite chlorophyll data show that the elevated chlorophyll concentrations in this region are consistently observed year after year and so are reflective of recurring large-scale wind- and circulation-induced productivity enhancement in the central equatorial Indian Ocean.

Item Details

Item Type:Refereed Article
Keywords:Indian Ocean, Yanai waves, moored observations, biogeochemistry, equator, Argo
Research Division:Earth Sciences
Research Group:Oceanography
Research Field:Physical Oceanography
Objective Division:Environment
Objective Group:Climate and Climate Change
Objective Field:Climate Variability (excl. Social Impacts)
Author:Strutton, PG (Associate Professor Peter Strutton)
Author:Phillips, HE (Dr Helen Phillips)
ID Code:92632
Year Published:2015
Funding Support:Australian Research Council (DP130102088)
Web of Science® Times Cited:6
Deposited By:IMAS Research and Education Centre
Deposited On:2014-06-24
Last Modified:2017-11-01
Downloads:338 View Download Statistics

Repository Staff Only: item control page