DocumentCode
407287
Title
Variability of Photosynthetically Usable Radiation in river-dominated coastal waters
Author
Dowell, Mark D. ; Campbell, Janet W. ; Salisbury, Joseph E. ; Moore, Timothy S.
Author_Institution
New Hampshire Univ., Durham, NH, USA
Volume
3
fYear
2003
fDate
22-26 Sept. 2003
Abstract
The present study considers, through the implementation of an optical river typology, the effect of the optical characteristics of different river plumes on estimates of Photosynthetically Available and Usable Radiation (PAR and PUR). The global distribution of waters influenced by the input of rivers is determined through the use of an Index of Fluvial Influence (IFI), which uses climatological salinity fields and hydrograph data for the world\´s 60 largest rivers. This IFI map is used as a template to extract spectral radiance data from ocean colour sensors. The radiance data is then analyzed using a fuzzy logic based classification scheme where the resulting classes are intended to represent the optical water types of globally distributed rivers. Each dataset of spectra clustered through the above classification, are inverted based on a nonlinear optimization routine and a multicomponent reflectance model including bidirectional effects. A second nonlinear optimization method using a published reflectance model was also included for comparison. The retrieved variables (backscattering coefficient at 555 nm, absorption of detrital material at 443 nm and the concentration of chlorophyll) provide the "typical" optical characteristics of the different water types to be used in the subsequent analysis. Typical Inherent Optical Properties (TOP) distributions and representative surface PAR distribution for subpolar, temperate and tropical regimes are used to estimate euphotic zone integrated PAR and PUR for the differing river optical water types. The effects of the TOPs in the differing water types affect two main aspects of PAR and PUR determination. The first influence is through the diffuse attenuation coefficient and thus the estimated euphotic depth itself, the second is the effect the relative proportions of different lOPs have on the conversion of downwelling irradiance to scalar irradiance (the relevant quantity for photosynthesis). Under certain, demonstrated, - > - > condition these two influences actually can counteract each other. Examples of high-resolution imagery, processed to retrieve derived PAR and PUR for three specific river plumes (Mississippi, Yangtze and Po), are also presented. Finally based on the above described sensitivity analysis, and using generic formulations for photosynthetic parameters, the impact of erroneously not accounting for the optical properties of river plumes in global calculations of primary production are estimated.
Keywords
fuzzy logic; oceanographic techniques; photosynthesis; rivers; sensitivity analysis; IFI; Index of Fluvial Influence; PAR; PUR; Photosynthetically Available Radiation; Photosynthetically Usable Radiation; TOP distribution; Typical Inherent Optical Properties; backscattering coefficient; bidirectional effect; chlorophyll concentration; climatological salinity field; detrital material; diffuse attenuation coefficient; downwelling irradiance; euphotic zone; fuzzy logic based classification scheme; high-resolution imagery; hydrograph data; multicomponent reflectance model; nonlinear optimization routine; ocean colour sensor; optical characteristics; optical river plume typology; published reflectance model; river input; river-dominated coastal water; scalar irradiance; sensitivity analysis; spectral radiance data; subpolar regime; subsequent analysis; temperate regime; tropical regime; variable retrieval; water global distribution; Data mining; Integrated optics; Nonlinear optics; Oceans; Optical attenuators; Optical sensors; Reflectivity; Rivers; Sea measurements; Water;
fLanguage
English
Publisher
ieee
Conference_Titel
OCEANS 2003. Proceedings
Conference_Location
San Diego, CA, USA
Print_ISBN
0-933957-30-0
Type
conf
DOI
10.1109/OCEANS.2003.178143
Filename
1282659
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