@article{fdi:010061763, title = {{B}iophysical responses near equatorial islands in the {W}estern {P}acific {O}cean during {E}l {N}ino/{L}a {N}ina transitions}, author = {{G}ierach, {M}. {M}. and {M}essie, {M}. and {L}ee, {T}. and {K}arnauskas, {K}. {B}. and {R}adenac, {M}arie-{H}{\'e}l{\`e}ne}, editor = {}, language = {{ENG}}, abstract = {{T}he biological response in the western equatorial {P}acific {O}cean during {E}l {N}ino/{L}a {N}ina transitions and the underlying physical mechanisms were investigated. {A} chlorophyll a bloom was observed near the {G}ilbert {I}slands during the 2010 {E}l {N}ino/{L}a {N}ina transition, whereas no bloom was observed during the 2007 {E}l {N}ino/{L}a {N}ina transition. {C}ompared to the previously observed bloom during the 1998 {E}l {N}ino/{L}a {N}ina transition, the 2010 bloom was weaker, lagged by 1-2 months, and was displaced eastward by similar to 200 km. {A}nalysis suggested that the occurrence, magnitude, timing, and spatial pattern of the blooms were controlled by two factors: easterly winds in the western equatorial {P}acific during the transition to {L}a {N}ina and the associated island mass effect that enhanced vertical processes (upwelling and vertical mixing), and the preconditioning of the thermocline depth and barrier layer thickness by the preceding {E}l {N}ino that regulated the efficiency of the vertical processes. {D}espite the similar strength of easterly winds in the western equatorial {P}acific during the 1998 and 2010 transitions to {L}a {N}ina, the 20092010 {E}l {N}ino prompted a deeper thermocline and thicker barrier layer than the 1997-1998 {E}l {N}ino that hampered the efficiency of the vertical processes in supplying nutrients from the thermocline to the euphotic zone, resulting in a weaker bloom.}, keywords = {{PACIFIQUE} ; {MICRONESIE} ; {GILBERT} {ILES}}, booktitle = {}, journal = {{G}eophysical {R}esearch {L}etters}, volume = {40}, numero = {20}, pages = {5473--5479}, ISSN = {0094-8276}, year = {2013}, DOI = {10.1002/2013gl057828}, URL = {https://www.documentation.ird.fr/hor/fdi:010061763}, }