GOPS Action 2014<\/em><\/span><\/h4>\u00a0<\/p>
Keywords<\/strong>\u00a0CDOM (Chromophotic Dissolved Organic Matter), water colour, MODIS satellite, Laucala Bay lagoon (Suva), New Caledonia lagoon, annual cycle, spectrofluorescence<\/p>Geographical area<\/strong>\u00a0South West Pacific, Fiji Islands, New Caledonia<\/p>Project sponsor<\/strong>\u00a0: C\u00e9cile Dupouy<\/a> (UMR MIO) Scientific Manager, CR1, Mediterranean Institute of Oceanography, (UM110) at Centre IRD Noum\u00e9a, 101 Promenade Roger Laroque, BP A5 - 98848 Noum\u00e9a Cedex, New Caledonia Tel: (687) 26.07.29.<\/p> <\/div> <\/div><\/section><\/div> Scientific objectives<\/h3>
\u00a0<\/p>
The countries of the South Pacific are highly dependent on their coastal zone for food security and tourism. Traditionally, there have been many conflicts between agriculture and mining. The challenges of maintaining the health (good biogeochemical balance) of coastal and coral environments are crucial.<\/p>
Chromophoric dissolved organic matter (CDOM) can carry contaminants and nutrient salts that have a major impact on the health of lagoon areas, even at great distances from the coast during heavy rainfall events. The DROPS project aims to :<\/p>
- an overall assessment of the CDOM's land-lagoon transfers to the world's largest enclosed lagoon in New Caledonia, and to the coastal areas of the Fiji Islands<\/li>
- Satellite mapping of CDOM plumes and feathers is based on daily MODIS 500 m Aqua\/Terra radiance data and made available via a geoportal.<\/li>
- CDOM spectrofluorescence measurements are used to characterise its components and identify its origin (mangroves, resuspension by seagrass beds, coral, terrigenous inputs linked to agricultural activity, PAH pollutants and anthropogenic tracers).<\/li><\/ol>
\u00a0<\/p>
Satellite maps Fiji Islands<\/h3>
\u00a0<\/p>
Daily CDOM maps from the American MODIS high-resolution water colour sensor (500 metres) repatriated from NASA were re-calculated using different regional algorithms (turbidity Ouillon et al., 2008, CDOM, Chla Wattelez et al., 2016), geographically re-projected onto the Fiji area and masked for land and clouds (in black) by a VALHYSAT processing chain (Dupouy, 2010; Lef\u00e8vre, 2010). The products are available online<\/a>.<\/p>Figure 1 (September 2002) shows the enrichments around the main island of Viti Levu for CDOM visible in the north-west and east of the island. Enrichment in small scattering particles (bbp (m-1)) is highest in the north-west. Chlorophyll enrichment extends further offshore, impacting a larger area around the islands and affecting coral zones over larger surfaces. Turbidity remains very low outside the lagoons, and very localised. To the south-east of Viti Levu, a plume localised near the coast (C) occurs southwards from Laucala Bay and is caused by the Ba River in heavy rain.<\/p>
\u00a0<\/p>
Geographical area<\/strong>\u00a0South West Pacific, Fiji Islands, New Caledonia<\/p> Project sponsor<\/strong>\u00a0: C\u00e9cile Dupouy<\/a> (UMR MIO) Scientific Manager, CR1, Mediterranean Institute of Oceanography, (UM110) at Centre IRD Noum\u00e9a, 101 Promenade Roger Laroque, BP A5 - 98848 Noum\u00e9a Cedex, New Caledonia Tel: (687) 26.07.29.<\/p> <\/div> <\/div><\/section><\/div> \u00a0<\/p> The countries of the South Pacific are highly dependent on their coastal zone for food security and tourism. Traditionally, there have been many conflicts between agriculture and mining. The challenges of maintaining the health (good biogeochemical balance) of coastal and coral environments are crucial.<\/p> Chromophoric dissolved organic matter (CDOM) can carry contaminants and nutrient salts that have a major impact on the health of lagoon areas, even at great distances from the coast during heavy rainfall events. The DROPS project aims to :<\/p> \u00a0<\/p> \u00a0<\/p> Daily CDOM maps from the American MODIS high-resolution water colour sensor (500 metres) repatriated from NASA were re-calculated using different regional algorithms (turbidity Ouillon et al., 2008, CDOM, Chla Wattelez et al., 2016), geographically re-projected onto the Fiji area and masked for land and clouds (in black) by a VALHYSAT processing chain (Dupouy, 2010; Lef\u00e8vre, 2010). The products are available online<\/a>.<\/p> Figure 1 (September 2002) shows the enrichments around the main island of Viti Levu for CDOM visible in the north-west and east of the island. Enrichment in small scattering particles (bbp (m-1)) is highest in the north-west. Chlorophyll enrichment extends further offshore, impacting a larger area around the islands and affecting coral zones over larger surfaces. Turbidity remains very low outside the lagoons, and very localised. To the south-east of Viti Levu, a plume localised near the coast (C) occurs southwards from Laucala Bay and is caused by the Ba River in heavy rain.<\/p> \u00a0<\/p>Scientific objectives<\/h3>
Satellite maps Fiji Islands<\/h3>