FN Archimer Export Format
PT J
TI Satellite observations of phytoplankton enrichments around seamounts in the South West Indian Ocean with a special focus on the Walters Shoal
BT 
AF Demarcq, Herve
   Noyon, Margaux
   Roberts, Michael J.
AS 1:1,2;2:3;3:3,4;
FF 1:;2:;3:;
C1 MARBEC, Univ Montpellier, CNRS, Ifremer, IRD, Sète, France
   Institut de Recherche pour le Développement (IRD), Marseille, France
   Ocean Science & Marine Food Security, Nelson Mandela University (NMU), Port Elizabeth, South Africa
   National Oceanography Centre (NOC), Southampton, United Kingdom
C2 IRD, FRANCE
   IRD, FRANCE
   UNIV NELSON MANDELA, SOUTH AFRICA
   NOC, UK
UM MARBEC
IN WOS Cotutelle UMR
   copubli-europe
   copubli-int-hors-europe
   copubli-sud
IF 2.732
TC 4
UR https://archimer.ifremer.fr/doc/00634/74577/74471.pdf
LA English
DT Article
CR MD 208 / WALTERS SHOAL
BO Marion Dufresne
DE ;SWIG;Chlorophyll-a;Remote sensing;MODIS-Aqua;Geostrophic currents;Deep chlorophyll maximum
AB Spatial anomalies associated with seamounts and islands have been detected in the South West Indian Ocean using a new surface chlorophyll-a based enrichment index (EI). Calculated from daily L3 4-km MODIS chl-a data from 2003 to 2018, the EI was used to quantify recurrent (seasonal) surface enrichment associated with these features. Most notable were the shallow Walters Shoal (18 m) and nearby deeper WS-2 seamount (480 m), both located on the southern Madagascar Ridge, which showed high EI values of 40% and 15% local enhancement. Tromelin Island, east of Madagascar, exhibited more moderate values of 15% local increase. Other shallower seamounts including La Pérouse (60 m) and MAD-Ridge (240 m) exhibited sporadic or no measurable surface maxima. Regions of strong mesoscale activity such as south of Madagascar where the South East Madagascar Current detaches from the continent also revealed high EI values. A marked seasonality of the EI was observed over the Walters Shoal, with higher values during the oligotrophic season than in the austral winter. The seasonal variability of the MLD in combination with the seamount bathymetry appears to induce the thermal and biological anomalies observed there, possibly favoured by the presence of a Taylor cap at the summit. Ship-collected in situ measurements showed the satellite observed enrichment to be associated with shallowing of the deep chlorophyll maximum, as well as a shift of phytoplankton groups towards diatoms and small flagellates. No net increase of integrated chl-a was measured but a potential doubling in primary productivity is expected. The EI developed in this study, designed to reveal sporadic, small localised chl-a maxima, is likely applicable to other areas in the ocean where there is local enrichments. 
PY 2020
PD JUL
SO Deep-sea Research Part Ii-topical Studies In Oceanography
SN 0967-0645
PU Elsevier BV
VL 176
UT 000556810400010
DI 10.1016/j.dsr2.2020.104800
ID 74577
ER

EF