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	<journal>
		<journal_title>Biogeosciences</journal_title>
		<journal_url>www.biogeosciences.net</journal_url>
		<issn>1726-4170</issn>
		<eissn>1726-4189</eissn>
		<volume_number>5</volume_number>
		<issue_number>2</issue_number>
		<publication_year>2008</publication_year>
	</journal>
	<doi>10.5194/bg-5-495-2008</doi>
	<article_url>http://www.biogeosciences.net/5/495/2008/</article_url>
	<abstract_html>http://www.biogeosciences.net/5/495/2008/bg-5-495-2008.html</abstract_html>
	<fulltext_pdf>http://www.biogeosciences.net/5/495/2008/bg-5-495-2008.pdf</fulltext_pdf>
	<start_page>495</start_page>
	<end_page>507</end_page>
	<publication_date>2008-04-07</publication_date>
	<article_title content_type="html">Particle optical backscattering along a chlorophyll gradient in the upper layer of the eastern South Pacific Ocean</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>Y. Huot</name>
			<email>huot@obs-vlfr.fr</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>A. Morel</name>
		</author>
		<author numeration="3" affiliations="2">
			<name>M. S. Twardowski</name>
		</author>
		<author numeration="4" affiliations="3">
			<name>D. Stramski</name>
		</author>
		<author numeration="5" affiliations="3">
			<name>R. A. Reynolds</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">CNRS, Laboratoire d&apos;Océanographie de Villefranche, 06230 Villefranche-sur-mer, France; Université Pierre et Marie Curie-Paris 6, Laboratoire d&apos;Océanographie de Villefranche, 06230 Villefranche-sur-mer, France</affiliation>
		<affiliation numeration="2" content_type="html">Department of Research, WET Labs, Inc., 165 Dean Knauss Dr., Narragansett, RI 02882, USA</affiliation>
		<affiliation numeration="3" content_type="html">Marine Physical Laboratory, Scripps Institution of Oceanography, University of California at San Diego, La Jolla, CA 92093-0238, USA</affiliation>
	</affiliations>
	<abstract content_type="html">The particulate scattering, &lt;i&gt;b&lt;/i&gt;&lt;sub&gt;p&lt;/sub&gt;, and backscattering, &lt;i&gt;b&lt;/i&gt;&lt;sub&gt;bp&lt;/sub&gt;,
coefficients are determined by the concentration and physical properties of
suspended particles in the ocean. They provide a simple description of the
influence of these particles on the scattering of light within the water
column. For the remote observation of ocean color, &lt;i&gt;b&lt;/i&gt;&lt;sub&gt;bp&lt;/sub&gt; along with the
total absorption coefficient govern the amount and spectral qualities of
light leaving the sea surface. However, for the construction and validation
of ocean color models measurements of &lt;i&gt;b&lt;/i&gt;&lt;sub&gt;bp&lt;/sub&gt; are still lacking, especially
at low chlorophyll &lt;i&gt;a&lt;/i&gt; concentrations ([Chl]). Here, we examine the
relationships between spectral &lt;i&gt;b&lt;/i&gt;&lt;sub&gt;bp&lt;/sub&gt; and &lt;i&gt;b&lt;/i&gt;&lt;sub&gt;p&lt;/sub&gt; vs. [Chl] along an 8000 km
transect crossing the Case 1 waters of the eastern South Pacific Gyre. In
these waters, over the entire range of [Chl] encountered (~0.02&amp;ndash;2 mg
m&lt;sup&gt;3&lt;/sup&gt;), both &lt;i&gt;b&lt;/i&gt;&lt;sub&gt;bp&lt;/sub&gt; and &lt;i&gt;b&lt;/i&gt;&lt;sub&gt;p&lt;/sub&gt; can be related to [Chl] by power
functions (i.e. &lt;i&gt;b&lt;/i&gt;&lt;sub&gt;p&lt;/sub&gt; or &lt;i&gt;b&lt;/i&gt;&lt;sub&gt;bp&lt;/sub&gt;=&amp;alpha;[Chl]&lt;sup&gt;&amp;beta;&lt;/sup&gt;). Regression analyses are carried out to provide
the parameters &amp;alpha; and &amp;beta; for several wavelengths throughout the
visible for both &lt;i&gt;b&lt;/i&gt;&lt;sub&gt;bp&lt;/sub&gt; and &lt;i&gt;b&lt;/i&gt;&lt;sub&gt;p&lt;/sub&gt;. When applied to the data, these
functions retrieve the same fraction of variability in &lt;i&gt;b&lt;/i&gt;&lt;sub&gt;bp&lt;/sub&gt; and &lt;i&gt;b&lt;/i&gt;&lt;sub&gt;p&lt;/sub&gt;
(coefficients of determination between 0.82 and 0.88). The &lt;i&gt;b&lt;/i&gt;&lt;sub&gt;bp&lt;/sub&gt;
coefficient fall within the bounds of previous measurements at intermediate
and high [Chl] recently published. Its dependence on [Chl] below
~0.1 mg m&lt;sup&gt;&amp;minus;3&lt;/sup&gt; is described for the first time with in situ data. The
backscattering ratio (i.e. &lt;i&gt;b&lt;/i&gt;&lt;sub&gt;bp&lt;/sub&gt;/&lt;i&gt;b&lt;/i&gt;&lt;sub&gt;p&lt;/sub&gt;) with values near 0.01 for all
stations appears to be spectrally neutral and not significantly dependent on
[Chl]. These results should foster the development of improved forward
models of the mean optical properties for oceanic Case 1 waters as well as
inverse models based upon them.</abstract>
	<references>
		<reference numeration="1" content_type="text">Ahn, Y. H., Bricaud, A., and Morel, A.: Light backscattering efficiency and related properties of some phytoplankters, Deep-Sea Res. Pt., 39, 1835&amp;ndash;1855, 1992. </reference>
		<reference numeration="2" content_type="text">Antoine, D., Morel, A., Gordon, H. R., Banzon, V. F., and Evans, R. H.: Bridging ocean color observations of the 1980s and 2000s in search of long-term trends, J. Geophys. Res., 110, C06009, doi:10.1029/2004JC002620, 2005. </reference>
		<reference numeration="3" content_type="text">Bader, H.: The hyperbolic distribution of particle sizes, J. Geophys. Res., 75, 2822&amp;ndash;2830, 1970. </reference>
		<reference numeration="4" content_type="text">Balch, W. M., Drapeau, D. T., Fritz, J. J., Bowler, B. C., and Nolan, J.: Optical backscattering in the arabian sea - continuous underway measurements of particulate inorganic and organic carbon, Deep-Sea Res. Pt. I, 48, 2423&amp;ndash;2452, 2001. </reference>
		<reference numeration="5" content_type="text">Behrenfeld, M. J., Boss, E., Siegel, D. A., and Shea, D. M.: Carbon-based ocean productivity and phytoplankton physiology from space, Global Biogeochem. Cy., 19, GB1006, doi:10.1029/2004GB002299, 2005. </reference>
		<reference numeration="6" content_type="text">Boss, E., Twardowski, M. S., and Herring, S.: Shape of the particulate beam attenuation spectrum and its inversion to obtain the shape of the particulate size distribution, Appl. Opt., 40, 4885&amp;ndash;4893, 2001. </reference>
		<reference numeration="7" content_type="text">Clark, G. L., and Ewing, G. C.: Remote spectroscopy of the sea for biological production studies, in: Optical aspect of oceanography, edited by: Jerlov, N. G., and Nielsen, E. S., Academic, New York, 494, 1974. </reference>
		<reference numeration="8" content_type="text">Gao, Y., Fan, S.-M., and Sarmiento, J. L.: Aeolian input to the ocean through precipitation scavenging: A modeling perspective and its implication for natural iron fertilization in the ocean, J. Geophys. Res., 108, 4221, doi:10.1029/2002JD002420, 2003. </reference>
		<reference numeration="9" content_type="text">Gordon, H. R., Brown, O. B., and Jacobs, M. M.: Computed relationships between inherent and apparent optical properties of a flat homogeneous ocean, Appl. Opt., 14, 417&amp;ndash;427, 1975. </reference>
		<reference numeration="10" content_type="text">Gordon, H. R. and Morel, A.: Remote assessment of ocean color for interpretation of satellite visible imagery: A review, Lecture notes on coastal and estuarine studies, Springer Verlag, Heidelberg, Germany, 114 pp., 1983. </reference>
		<reference numeration="11" content_type="text">Gordon, H. R., Brown, O. B., Evans, R. H., Brown, J. W., Smith, R. C., Baker, K. S., and Clark, D. K.: A semianalytic radiance model of ocean color, J. Geophys. Res., 93, 10 909&amp;ndash;10 924, 1988. </reference>
		<reference numeration="12" content_type="text">IOCCG: Remote sensing of inherent optical properties: Fundamentals, tests of algorithms, and applications, in: Reports of the International Ocean-Colour Coordinating Group, edited by: Lee, Z.-P., No. 5, IOCCG, Dartmouth, Canada, 126, 2006. </reference>
		<reference numeration="13" content_type="text">Lee, Z. P., Carder, K. L., and Arnone, R. A.: Deriving inherent optical properties from water color: A multiband quasi-analytical algorithm for optically deep waters, Appl. Opt., 41, 5755&amp;ndash;5772, 2002. </reference>
		<reference numeration="14" content_type="text">Loisel, H. and Morel, A.: Light scattering and chlorophyll concentration in case 1 waters: A reexamination, Limnol. Oceanogr., 43, 847&amp;ndash;858, 1998. </reference>
		<reference numeration="15" content_type="text">Maritorena, S., Siegel, D. A., and Peterson, A. R.: Optimization of a semianalytical ocean color model for global-scale applications, Appl. Opt., 41, 2705&amp;ndash;2714, 2002. </reference>
		<reference numeration="16" content_type="text">Morel, A.: Diffusion de la lumière par les eaux de mer. Resultats expérimentaux et approche théorique., AGARD lectures series, 3.1.1&amp;ndash;3.1.76, 1973. </reference>
		<reference numeration="17" content_type="text">Morel, A. and Prieur, L.: Analysis of variations in ocean color, Limnol. Oceanogr., 22, 709&amp;ndash;722, 1977. </reference>
		<reference numeration="18" content_type="text">Morel, A. and Bricaud, A.: Theoretical results concerning the optics of phytoplankton, with special references to remote sensing applications, in: Oceanography from space, edited by: Gower, J. F. R., Plenum, New York, 313&amp;ndash;327, 1981. </reference>
		<reference numeration="19" content_type="text">Morel, A. and Bricaud, A.: Inherent properties of algal cells including picoplankton: Theoretical and experimental results., in: Photosynthetic picoplankton, edited by: Platt, T. and Li, W. K. W., Canadian bulletin of fisheries and aquatic sciences, 521&amp;ndash;559, 1986. </reference>
		<reference numeration="20" content_type="text">Morel, A.: Optical modeling of the upper ocean in relation to its biogenous matter content (case 1 waters), J. Geophys. Res., 93, 10 749&amp;ndash;10 768, 1988. </reference>
		<reference numeration="21" content_type="text">Morel, A. and Ahn, Y.-H.: Optics of heterotrophic nanoflagellates and ciliates: A tentative assessment of their scattering role in oceanic waters compared to those of bacterial and algal cells, J. Mar. Res., 49, 177&amp;ndash;202, 1991. </reference>
		<reference numeration="22" content_type="text">Morel, A. and Maritorena, S.: Bio-optical properties of oceanic waters: A reappraisal, J. Geophys. Res., 106, 7163&amp;ndash;7180, 2001. </reference>
		<reference numeration="23" content_type="text">Morel, A., Gentili, B., Chami, M., and Ras, J.: Bio-optical properties of high chlorophyll case 1 waters and of yellow-substance-dominated case 2 waters, Deep-Sea Res. Pt. I, 53, 1439&amp;ndash;1459, 2006. </reference>
		<reference numeration="24" content_type="text">Morel, A., Gentili, B., Claustre, H., Babin, M., Bricaud, A., Ras, J., and Tièche, F.: Optical properties of the &quot;Clearest&quot; Natural waters, Limnol. Oceanogr., 52, 217&amp;ndash;229, 2007. </reference>
		<reference numeration="25" content_type="text">O&apos;Reilly, J. E., Maritorena, S., Mitchell, B. G., Siegel, D. A., Carder, K. L., Garver, S. A., Kahru, M., and McClain, C. R.: Ocean color chlorophyll algorithms for SeaWiFS, J. Geophys. Res., 103, 24 937&amp;ndash;24 953, 1998. </reference>
		<reference numeration="26" content_type="text">Petzold, T. J.: Volume scattering functions for selected ocean waters, Scripps Institution of Oceanography, Visibility Lab, San Diego, 85, 1972. </reference>
		<reference numeration="27" content_type="text">Ras, J., Claustre, H., and Uitz, J.: Spatial variability of phytoplankton pigment distributions in the subtropical South Pacific ocean: Comparison between in situ and predicted data, Biogeosciences, 5, 353&amp;ndash;369, 2007. </reference>
		<reference numeration="28" content_type="text">Reynolds, R. A., Stramski, D., and Mitchell, B. G.: A chlorophyll-dependent semianalytical reflectance model derived from field measurements of absorption and backscattering coefficients within the southern ocean, J. Geophys. Res., 106, 7125&amp;ndash;7138, 2001. </reference>
		<reference numeration="29" content_type="text">Snyder, W. A., Arnone, R. A., Davis, C. O., Goode, W., Gould, R. W., Ladner, S., Lamela, G., Rhea, W. J., Stavn, R., Sydor, M., and Weidemann, A.: Optical scattering and backscattering by organic and inorganic particulates in U.S. Coastal waters, Appl. Opt., 47, 666&amp;ndash;677, 2008. </reference>
		<reference numeration="30" content_type="text">Stramska, M., Stramski, D., Hapter, R., Kaczmarek, S., and Ston, J.: Bio-optical relationships and ocean color algorithms for the north polar region of the Atlantic, J. Geophys. Res., 108, 3143, doi:10.1029/2001JC001195, 2003. </reference>
		<reference numeration="31" content_type="text">Stramska, M., Stramski, D., Kaczmarek, S., Allison, D. B., and Schwarz, J.: Seasonal and regional differentiation of bio-optical properties within the north polar Atlantic, J. Geophys. Res., 111, C08003, doi:10.1029/2005JC003293, 2006. </reference>
		<reference numeration="32" content_type="text">Stramski, D. and Kiefer, D. A.: Light scattering by microorganisms in the open ocean, Prog. Oceanogr., 28, 343&amp;ndash;383, 1991. </reference>
		<reference numeration="33" content_type="text">Stramski, D., Boss, E., Bogucki, D., and Voss, K. J.: The role of seawater constituents in light backscattering in the ocean, Prog. Oceanogr., 61, 27&amp;ndash;56, 2004. </reference>
		<reference numeration="34" content_type="text">Stramski, D., Reynolds, R. A., Babin, M., Kaczmarek, S., Lewis, M. R., Röttgers, M., Sciandra, A., Stramska, M., Twardowski, M. S., Franz, B. A., and Claustre, H.: Relationships between the surface concentration of particulate organic carbon and optical properties in the eastern South Pacific and eastern Atlantic oceans., Biogeosciences, 5, 171&amp;ndash;201, 2008. </reference>
		<reference numeration="35" content_type="text">Sullivan, J. M., Twardowski, M. S., Donaghay, P. L., and Freeman, S. A.: Use of optical scattering to discriminate particle types in coastal waters, Appl. Opt., 44, 1667&amp;ndash;1680, 2005. </reference>
		<reference numeration="36" content_type="text">Twardowski, M. S., Boss, E., Macdonald, J. B., Pegau, W. S., Barnard, A. H., and Zaneveld, J. R. V.: A model for estimating bulk refractive index from the optical backscattering ratio and the implications for understanding particle composition in case i and case ii waters, J. Geophys. Res., 106, 14 129&amp;ndash;14 142, 2001. </reference>
		<reference numeration="37" content_type="text">Twardowski, M. S., Claustre, H., Freeman, S. A., Stramski, D., and Huot, Y.: Optical backscattering properties of the &quot;clearest&quot; natural waters, Biogeosciences, 4, 1041&amp;ndash;1058, 2007. </reference>
		<reference numeration="38" content_type="text">Ulloa, O., Sathyendranath, S., and Platt, T.: Effect of the particle-size distribution on the backscattering ratio in seawater, Appl. Opt., 33, 7070&amp;ndash;7077, 1994. </reference>
		<reference numeration="39" content_type="text">Whitmire, A. L., Boss, E., Cowles, T. J., and Pegau, W. S.: Spectral variability of the particulate backscattering ratio, Opt. Express., 15, 7019&amp;ndash;7031, 2007. </reference>
	</references>
</article>
