FN Archimer Export Format
PT J
TI Phytoplankton spring and fall blooms in the North Atlantic in the 1980s and 2000s
BT 
AF MARTINEZ, Elodie
   ANTOINE, David
   D'ORTENZIO, Fabrizio
   DE BOYER MONTEGUT, Clement
AS 1:1;2:1;3:1;4:2;
FF 1:;2:;3:;4:PDG-ODE-LOS;
C1 Univ Paris, Lab Oceanog Villefranche, UMR 7093, CNRS,UPMC, F-06230 Villefranche Sur Mer, France.
   IFREMER, Ctr Brest, Lab Oceanog Spatiale, F-29280 Plouzane, France.
C2 UNIV PARIS 06, FRANCE
   IFREMER, FRANCE
SI BREST
SE PDG-ODE-LOS
IN WOS Ifremer jusqu'en 2018
   copubli-france
   copubli-univ-france
IF 3.021
TC 47
UR https://archimer.ifremer.fr/doc/00054/16556/14070.pdf
LA English
DT Article
AB Phytoplankton chlorophyll-a (Chl) seasonal cycles of the North 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. It covers latitudes from 30 degrees N-50 degrees N and longitudes from 60 degrees W-0 degrees W, where 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 in the eastern Atlantic (east of 40 degrees W), because of a delayed deepening of the mixed layer at the end of summer (mixed layer depth (MLD) determined from in situ data). Conversely, the spring bloom of the eastern Atlantic was stronger in the 2000s than it was in the 1980s, because of a deeper MLD and stronger winds in winter. In the Northwestern Atlantic (northwest of 38 degrees N-40 degrees W), little differences are observed for spring and fall blooms, and for the wintertime MLD. 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.
PY 2011
PD NOV
SO Journal Of Geophysical Research-oceans
SN 0148-0227
PU Amer Geophysical Union
VL 116
IS C11029
UT 000297271900001
DI 10.1029/2010JC006836
ID 16556
ER

EF