@article{fdi:010077333, title = {{R}ole of iron in the {M}arquesas {I}sland mass effect}, author = {{R}aapoto, {H}. and {M}artinez, {E}lodie and {P}etrenko, {A}. and {D}oglioli, {A}. and {G}orgues, {T}homas and {S}auzede, {R}. and {M}aamaatuaiahutapu, {K}. and {M}aes, {C}hristophe and {M}enk{\`e}s, {C}hristophe and {L}efevre, {J}{\'e}r{\^o}me}, editor = {}, language = {{ENG}}, abstract = {{A} remarkable chlorophyll-a concentration ({C}hl, a proxy of phytoplankton biomass) plume can be noticed on remotely sensed ocean color observations at the boundary separating the equatorial mesotrophic from the subtropical oligotrophic waters in the central {S}outh {P}acific {O}cean. {T}his prominent biological feature is known as the island mass effect of the {M}arquesas archipelago. {W}aters surrounding these islands present high macronutrient concentrations but an iron depletion. {I}n this study, the origin of {C}hl enhancement is investigated using a modeling approach. {F}our simulations based on identical physical and biogeochemical forcings but with different iron sources are conducted and analyzed. {O}nly simulations considering an iron input from the island sediments present similar patterns (despite being too weak) of vertical and horizontal {C}hl distributions as compared to biogeochemical-{A}rgo profiling float and satellite observations. {I}n addition, simulations with no other iron input than the boundary forcings reveal the relative importance of remote processes in modulating the seasonal pattern of {C}hl around the archipelago through horizontal advection of nutrient-rich waters from the equator toward the archipelago and vertical mixing uplifting deep nutrient-rich waters toward the upper lit layer.}, keywords = {{PACIFIQUE} ; {MARQUISES}}, booktitle = {}, journal = {{J}ournal of {G}eophysical {R}esearch : {O}ceans}, volume = {124}, numero = {11}, pages = {7781--7796}, ISSN = {2169-9275}, year = {2019}, DOI = {10.1029/2019jc015275}, URL = {https://www.documentation.ird.fr/hor/fdi:010077333}, }