<?xml version='1.0' encoding='utf-8'?>
<oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:contributor>L.A.K. Mertes</dc:contributor>
  <dc:contributor>D.A. Siegel</dc:contributor>
  <dc:contributor>C. Mackenzie</dc:contributor>
  <dc:creator>J.A. Warrick</dc:creator>
  <dc:date>2004</dc:date>
  <dc:description>A technique is presented for estimating suspended sediment concentrations of turbid coastal waters with remotely sensed multi-spectral data. The method improves upon many standard techniques, since it incorporates analyses of multiple wavelength bands (four for Sea-viewing Wide Field of view Sensor (SeaWiFS)) and a nonlinear calibration, which produce highly accurate results (expected errors are approximately ±10%). Further, potential errors produced by erroneous atmospheric calibration in excessively turbid waters and influences of dissolved organic materials, chlorophyll pigments and atmospheric aerosols are limited by a dark pixel subtraction and removal of the violet to blue wavelength bands. Results are presented for the Santa Barbara Channel, California where suspended sediment concentrations ranged from 0–200+ mg l&lt;sup&gt;−1&lt;/sup&gt; (±20 mg l&lt;sup&gt;−1&lt;/sup&gt;) immediately after large river runoff events. The largest plumes were observed 10–30 km off the coast and occurred immediately following large El Niño winter floods.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1080/01431160310001619535</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Taylor &amp; Francis</dc:publisher>
  <dc:title>Estimating suspended sediment concentrations in turbid coastal waters of the Santa Barbara Channel with SeaWiFS</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>