In spring, 2001 a NASA high altitude ER-2 aircraft flew missions over coastal Louisiana to monitor suspended sediment patterns in and around the Atchafalaya Bay region of Louisiana. The Atchafalaya Bay is a sediment rich zone of the coastal region, especially in spring when snowmelt and spring rains annually swell the volume of the river discharge into the bay. The coastal sediment influx is distributed by micro tidal influences and wind driven currents in the nearshore zone, accumulating on the shallow subaqueous bottom or remaining in suspension over long distances in the prevailing currents. The ER-2 flights were timed to be coincident with the late morning overpass of the MODIS instrument on Terra. By co-locating MODIS 250m resolution data with MAS (50m resolution) on the ER-2, an effort is underway to establish a coastal suspended sediment concentration product for high sediment coastal regions (type 2 waters). The initial step toward this goal was taken with the spring 2001 ER-2 flights and a boat team collecting in situ and hand-held radiometer measurements. The ground-based measurements form the basis of a suspended sediment concentration estimation algorithm. Transferring this algorithm to MODIS will lead to routine estimation of suspended sediment concentration for coastal sites spread around the globe.
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