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Analysis of apparent optical properties and ocean color models using measurements of seawater constituents in New England continental shelf surface waters
- Source :
- Journal of Geophysical Research: Oceans. 109
- Publication Year :
- 2004
- Publisher :
- American Geophysical Union (AGU), 2004.
-
Abstract
- Received 22 May 2003; revised 10 December 2003; accepted 14 January 2004; published 17 March 2004. [1] We used budgets of absorption (a), scattering (b), and backscattering (bb) for particles and chromophoric dissolved organic matter (CDOM) to investigate sources of seasonal variations in apparent optical properties (AOPs) of New England continental shelf surface waters. Spectral a, b, and bb budgets for particles were estimated from flow cytometric measurements of eukaryotic pico/nanophytoplankton, Synechococcus, heterotrophic prokaryotes, detritus, and minerals; AOPs were modeled with Hydrolight radiative transfer software. For late summer and spring, our modeled values of the diffuse attenuation coefficient (Kd) and remote sensing reflectance (Rrs) were on average within 15% and 9%, respectively, of independent measurements. This close agreement allowed us to examine how different seawater constituents contributed to AOP variability. Higher values of Kd in the spring, compared to summer, were due to higher absorption by eukaryotic phytoplankton (aeuk) and CDOM (aCDOM), which coincided with higher nutrient levels and less stratified conditions than in the summer. Differences in the spectral shape of Rrs between the seasons were caused by a combination of differences in aeuk, aCDOM, and bb from non-phytoplankton particles (minerals and detritus combined). For nonphytoplankton bb the major seasonal difference was a higher inverse wavelength dependence in the summer due to the effects of small organic detritus. We applied two semianalytical ocean color models to our data, in order to evaluate whether the assumptions and parameterizations inherent in these models are applicable for New England shelf waters. We show how differences between observed and modeled chlorophyll a specific phytoplankton absorption, aCDOM, and non-phytoplankton bb cause errors in chlorophyll a concentration and IOPs retrieved from reflectance inversion models. INDEX TERMS: 4847 Oceanography: Biological and Chemical: Optics; 4219 Oceanography: General: Continental shelf processes; 4275 Oceanography: General: Remote sensing and electromagnetic processes (0689); 4227 Oceanography: General: Diurnal, seasonal, and annual cycles; KEYWORDS: optical properties, suspended particulate matter, ocean color Citation: Green, R. E., and H. M. Sosik (2004), Analysis of apparent optical properties and ocean color models using measurements of seawater constituents in New England continental shelf surface waters, J. Geophys. Res., 109, C03026
- Subjects :
- Atmospheric Science
Chlorophyll a
Soil Science
Aquatic Science
Oceanography
chemistry.chemical_compound
Geochemistry and Petrology
Nanophytoplankton
Phytoplankton
Earth and Planetary Sciences (miscellaneous)
Earth-Surface Processes
Water Science and Technology
geography
geography.geographical_feature_category
Detritus
Ecology
Continental shelf
Paleontology
Forestry
Colored dissolved organic matter
Geophysics
chemistry
Space and Planetary Science
Ocean color
Environmental science
Seawater
Subjects
Details
- ISSN :
- 01480227
- Volume :
- 109
- Database :
- OpenAIRE
- Journal :
- Journal of Geophysical Research: Oceans
- Accession number :
- edsair.doi...........45c0e1bbdb49affa7bf25b5ee96ae3af
- Full Text :
- https://doi.org/10.1029/2003jc001977