Abstract
Phytoplankton chlorophyll-a (Chl) seasonal cycles of the Northeastern Atlantic are described using satellite ocean color observations covering the 1980s and the 2000s. The study region is where warmer SST and higher Chl in the 2000s as compared to the 1980s have been reported (30°–50° N and 40°–0° W). In this area, two phytoplankton blooms take place: a spring bloom that follows stratification of upper layers, and a fall bloom due to nutrient entrainment through deepening of the mixed layer. In the 1980s, spring and fall blooms were of similar amplitude over the entire study region. In the 2000s, the fall bloom was weaker likely due to a delayed deepening of the mixed layer at the end of summer (mixed-layer depths—MLD—determined from in situ data). Conversely, the spring bloom was stronger in the 2000s than it was in the 1980s, in parallel to a deeper MLD and stronger winds in winter. Our results show that the links between upper-layer stratification, SST changes, and biological responses are more complex than the simple paradigm that sequentially relates higher stratification with warmer SST and an enhanced (weakened) growth of the phytoplankton population in the subpolar (subtropical) region.
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Acknowledgments
EM was supported by the Changing Earth Science Network initiative funded by the Support To Science Element (STSE) program of the European Space Agency (ESA). This work was supported by the Centre National d’EtudesSpatiales (CNES).
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Martinez, E., Antoine, D., D’Ortenzio, F., DeBoyerMontégut, C. (2013). DecPhy—Variability of the Phytoplankton Spring and Fall Blooms in the Northeastern Atlantic in the 1980s and 2000s. In: Remote Sensing Advances for Earth System Science. SpringerBriefs in Earth System Sciences. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-32521-2_6
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DOI: https://doi.org/10.1007/978-3-642-32521-2_6
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