<?xml version='1.0' encoding='utf-8'?>
<oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:contributor>Shubha Sathyendranath</dc:contributor>
  <dc:contributor>Trevor Platt</dc:contributor>
  <dc:creator>John Brock</dc:creator>
  <dc:date>1993</dc:date>
  <dc:description>&lt;p&gt;Seasonal changes in mixed-layer depth and phytoplankton biomass in the Arabian Sea are assessed with climatologies of ship-based hydrographic measurements and ocean-color observations from satellite. &amp;nbsp;At the close of the intermonsoons in November and especially May, the open Arabian Sea resembles the stereotypic, unperturbed tropical ocean, with a thin oligotrophic mixed layer and a pronounced subsurface chlorophyll maximum. &amp;nbsp;Both the northeast and southwest monsoons disrupt this typical tropical hydrography through mixed-layer deepening and eutrophication in the central and northern Arabian Sea. &amp;nbsp;Computations using a spectral model of light penetration suggest that seasonal changes in mixed-layer thickness and phytoplankton concentration result in pronounced fluctuations through the annual cycle in the radiant flux reaching the base of the mixed layer. &amp;nbsp;At the close of the fall and spring intermonsoons the base of the model euphotic zone is in the thermocline across all of the open Arabian Sea. &amp;nbsp;The euphotic zone appears to rise into the mixed layer of the northern Arabian Sea during both the winter and summer monsoons. &amp;nbsp;Strong seasonality in total primary production and its partitioning between the mixed layer and thermocline is predicted byb a photo-synthesis-irradiance model for a site in the western Arabian Sea (14.36&lt;span&gt;&amp;deg; N, 57.38&amp;deg; E). &amp;nbsp;Modeled mixed-layer primary production depicts an intense peak for the southwest monsoon and a secondary northeast monsoon peak separated by intermonsoon period of low production. &amp;nbsp;During the fall and spring intermonsoons, in the presence of a subsurface clorophyll maximum, the model estimate of primary production in the thermocline exceeds that in the mixed layer. &amp;nbsp;Our model calculations suggest that the subsurface clorophyll maximum present in the Arabian Sea during the spring intermonsoon is a precursor of the regional, summer, phytoplankton bloom.&lt;/span&gt;&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.3354/meps101209</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Inter-Research Science Publisher</dc:publisher>
  <dc:title>Modelling the seasonality of subsurface light and primary production in the Arabian Sea</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>