Poster's note : This new dataset may be of interest to those studying OIF

http://onlinelibrary.wiley.com/doi/10.1111/gcb.12457/abstract

>From silk to satellite: half a century of ocean colour anomalies in the
Northeast Atlantic

D.E. Raitsos, Y. Pradhan, S.J. Lavender, I. Hoteit, A.
McQuatters-Gollop, P. C Reid, A. J Richardson

DOI: 10.1111/gcb.12457

Keywords:

phytoplankton variability;chlorophyll;ocean colour;northern hemisphere
temperature;Northeast Atlantic

Abstract

Changes in phytoplankton dynamics influence marine biogeochemical cycles,
climate processes, and food webs, with substantial social and economic
consequences. Large-scale estimation of phytoplankton biomass was possible
via ocean colour measurements from two remote sensing satellites – the
Coastal Zone Color Scanner (CZCS, 1979-1986) and the Sea-viewing Wide
Field-of-view Sensor (SeaWiFS, 1998-2010). Due to the large gap between the
two satellite eras and differences in sensor characteristics, comparison of
the absolute values retrieved from the two instruments remains challenging.
Using a unique in situ ocean colour dataset that spans more than half a
century, the two satellite-derived chlorophyll-a (Chl-a) eras are linked to
assess concurrent changes in phytoplankton variability and bloom timing
over the Northeast Atlantic Ocean and North Sea. Results from this unique
re-analysis reflect a clear increasing pattern of Chl-a, a merging of the
two seasonal phytoplankton blooms producing a longer growing season and
higher seasonal biomass, since the mid-1980s. The broader climate plays a
key role in Chl-a variability as the ocean colour anomalies parallel the
oscillations of the Northern Hemisphere Temperature (NHT) since 1948.

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