Shutdown of convection triggers increase of surface chlorophyll

The long-standing explanation of the triggering cause of the surface increase of phytoplankton visible in spring satellite images argues that phytoplankton biomass accumulation begins once the mixed layer depths become shallower than a ‘critical depth’. However, a series of recent studies have found...

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Bibliografiska uppgifter
Huvudupphovsmän: Ferrari, Raffaele, Taylor, John R., Merrifield, Sophia Tiare
Övriga upphovsmän: Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences
Materialtyp: Artikel
Språk:en_US
Publicerad: Elsevier 2015
Länkar:http://hdl.handle.net/1721.1/97881
https://orcid.org/0000-0002-3736-1956
https://orcid.org/0000-0002-4152-7285