@incollection{fdi:010063837,
  title = {{I}nfluence of {CDOM} and {P}article {C}omposition on {O}cean {C}olor of the {E}astern {N}ew {C}aledonia {L}agoon during the {CALIOPE} {C}ruises},
  author = {{D}upouy, {C}{\'e}cile and {R}{\¨o}ttgers, {R}. and {T}edetti, {M}. and {M}artias, {C}hlo{\'e} and {M}urakami, {H}. and {D}oxaran, {D}. and {L}antoine, {F}. and {R}odier, {M}artine and {F}avareto, {L}. and {K}ampel, {M}. and {G}outx, {M}. and {F}rouin, {R}.},
  editor = {},
  language = {{ENG}},
  abstract = {{O}cean color of tropical lagoons is dependent on bathymetry and bottom type, as well as input of coastal living and mineral particles and chromophoric dissolved organic matter ({CDOM}). {T}he {N}ew {C}aledonia lagoon lies in the {S}outhwestern {T}ropical {P}acific around 21° 30’{S} and 166° 30’{E}, with a great marine biodiversity in {UNESCO} {H}eritage coral reefs, benthic sea grass, and benthic communities. {T}hey are largely connected to the open ocean in the southern and eastern parts, but only by narrow passes in the southwest part. {T}he trophic state is linked to spatial variations in flushing times. {H}igh run offs due to rain carrying abundant chromophoric dissolved organic matter ({CDOM}) and particle loads may greatly impact the functioning of ecosystems while rivers and sewage effluents may induce localized impacts. {T}wo oceanographic cruises ({CALIOPE} 1 in 2011 and {CALIOPE} 2 in 2014) were carried out off the {E}astern {C}oast of {N}ew {C}aledonia during a calm dry period and during high winds, respectively. {M}ulti- and hyper-spectral marine reflectance was measured with a {SIMBADA} instrument and a {TRIOS} radiometer system, together with inherent optical properties (total and {CDOM} absorption coefficients with a {PSICAM}, in situ absorption and scattering with an {AC}9, backscattering with a {H}ydroscat-6). {F}luorescence of {CDOM} ({EEM}/{PARAFAC}) was measured on collected 0.2 μm filtered samples. {I}n 2014, {S}atlantic and {F}ield{S}pec hyper-spectral radiometers were available for in-water profiling of upwelling radiance and downwelling irradiance and above-water reflectance measurements, respectively. {I}nherent and apparent optical data from the two cruises are compared and used to estimate ocean color algorithms performance and evaluate a {L}inear {M}atrix {I}nversion method, providing tools for remote sensing on this highly under-sampled coastal region of {N}ew {C}aledonia.},
  keywords = {{TELEDETECTION} {SPATIALE} ; {DONNEES} {SATELLITE} ; {CAMPAGNE} {OCEANOGRAPHIQUE} ; {LAGON} ; {ZONE} {TROPICALE} ; {PHYTOPLANCTON} ; {MATIERE} {ORGANIQUE} {DISSOUTE} ; {REFLECTANCE} ; {COULEUR} {DE} {L}'{OCEAN} ; {CDOM} ; {RADIOMETRE} {TRIOS} ; {CALIOPE} ; {NOUVELLE} {CALEDONIE}},
  booktitle = {{O}cean remote sensing and monitoring from space},
  volume = {9261},
  numero = {92610{M}},
  pages = {92610{M}/1--92610{M}/8},
  address = {{B}ellingham {WA}},
  publisher = {{SPIE}},
  series = {{P}roceedings of {SPIE}},
  year = {2014},
  DOI = {10.1117/12.2073309},
  ISSN = {0277-786{X}},
  URL = {https://www.documentation.ird.fr/hor/fdi:010063837},
}