@article{fdi:010079370,
  title = {{C}ontrasted contribution of intraseasonal time scales to surface chlorophyll variations in a bloom and an oligotrophic regime},
  author = {{K}eerthi, {M}. {G}. and {L}evy, {M}arina and {A}umont, {O}livier and {L}engaigne, {M}atthieu and {A}ntoine, {D}.},
  editor = {},
  language = {{ENG}},
  abstract = {{U}nderstanding long-term variations of ocean ecosystems requires untangling the time scales involved in their natural fluctuations. {W}e applied a temporal decomposition procedure to two decades of satellite ocean color observations to characterize the time variability of surface chlorophyll-a ({SC}hl) in the {M}editerranean {S}ea. {I}n order to assess the reliability of the satellite data at capturing intraseasonal, seasonal, and interannual variability, we first show that satellite {SC}hl data compare well with field data of chlorophyll-a fluorescence from the long-term {BOUSSOLE} time series, at all three time scales. {T}he decomposition procedure is then applied to satellite {SC}hl and to mixing-layer depth ({M}x{LD}) data from an ocean reanalysis, both at the scale of the entire {M}editerranean {S}ea. {O}ur results reveal similar amplitude for the seasonal and intraseasonal {SC}hl variations in the northwestern bloom region, together explaining about 90% of the {SC}hl variance. {C}oherent seasonal {SC}h{I} variations occur at the scale of the bloom region (similar to 400 km) and are tightly connected with seasonal {M}x{LD} changes. {I}ntraseasonal {SC}hl fluctuations occur at smaller spatial scales (similar to 100 km), suggesting they would he generated by storms although they weakly correlate to variations of the {M}x{LD} reanalysis. {O}ver the oligotrophic part of the {M}editerranean {S}ea, about 80% of the variability in both {SC}hl and {M}x{LD} are explained by basin-scale (similar to 1,000 km) seasonal variations. {I}ntraseasonal variability occurs at much smaller spatial scales, typical of mesoscale activity (similar to 30 km). {T}hese results support the hypothesis that seasonal {SC}h{I} variations are driven by changes in {M}x{LD}, while mesoscale activity and storms drive the intraseasonal {SC}hl fluctuations. {P}lain {L}anguage {S}ummary {I}n the context of our changing climate, an ongoing challenge is to be able to reliably detect and attribute trends in ocean color records of surface chlorophyll-a ({SC}hl), which is the only observable variable representative of the state of marine ecosystem available at global scale. {H}owever, the magnitude of the natural variability of {SC}hl is much stronger than that of the {SC}hl long-term trend. {F}urthermore, this natural variability occurs over a large range of unrelated time scales, making it difficult to detect and attribute a climate-driven trend. {H}ere we focus on the variability over temporal scales that have been overlooked because their observation requires continuous measurements, that is, fluctuations that are shorter than seasonal ones. {I}n the case of the {M}editerranean {S}ea, we show that such intraseasonal variations can be as large as seasonal ones and that they may also be less predictable because they likely ensue from processes such as storms or ocean eddies.},
  keywords = {{MEDITERRANEE}},
  booktitle = {},
  journal = {{J}ournal of {G}eophysical {R}esearch : {O}ceans},
  volume = {125},
  numero = {5},
  pages = {e2019{JC}015701 [18 ]},
  ISSN = {2169-9275},
  year = {2020},
  DOI = {10.1029/2019jc015701},
  URL = {https://www.documentation.ird.fr/hor/fdi:010079370},
}